ࡱ> JLEFGHIc ):jbjbSS 5116#]d@ , /$$"FFF%%%.......,12.%!%%%.(FF$(((% 8FF.lt%.((.. Gߺ!.U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY WIDE-ANGLE SEISMIC RECORDINGS FROM THE 2002 GEORGIA BASIN GEOHAZARDS INITIATIVE, NORTHWESTERN WASHINGTON AND BRITISH COLUMBIA By Thomas M. Brocher1, Thomas L. Pratt2, George D. Spence3, Michael Riedel4, and Roy D. Hyndman4 Open-File Report 03-160 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, product or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1U.S. Geological Survey, 345 Middlefield Road, M/S 977, Menlo Park, CA 94025 2U.S. Geological Survey, School of Oceanography, Box 357940, Univ. Wash., Seattle, WA 98195 3School of Earth and Ocean Sci., Univ. of Victoria, Victoria, B.C., V8W 2Y2, Canada 4Pacific Geoscience Centre, Geol. Survey of Canada, Sidney, B.C., V8L 4B2, Canada 2003 ABSTRACT This report describes the acquisition and processing of shallow-crustal wide-angle seismic-reflection and refraction data obtained during a collaborative study in the Georgia Strait, western Washington and southwestern British Columbia. The study, the 2002 Georgia Strait Geohazards Initiative, was conducted in May 2002 by the Pacific Geoscience Centre, the U.S. Geological Survey, and the University of Victoria. The wide-angle recordings were designed to image shallow crustal faults and Cenozoic sedimentary basins crossing the International Border in southern Georgia basin and to add to existing wide-angle recordings there made during the 1998 SHIPS experiment. We recorded, at wide-angle, 800 km of shallow penetration multichannel seismic-reflection profiles acquired by the Canadian Coast Guard Ship (CCGS) Tully using an air gun with a volume of 1.967 liters (120 cu. in.). Prior to this reflection survey, we deployed 48 Refteks onshore to record the airgun signals at wide offsets. Three components of an oriented, 4.5 Hz seismometer were digitally recorded at all stations. Nearly 160,300 individual air gun shots were recorded along 180 short seismic reflection lines. In this report, we illustrate the wide-angle profiles acquired using the CCGS Tully, describe the land recording of the air gun signals, and summarize the processing of the land recorder data into common-receiver gathers. We also describe the format and content of the archival tapes containing the SEGY-formated, common-receiver gathers for the Reftek data. Data quality is variable but the experiment provided useful data from 42 of the 48 stations deployed. Three-fourths of all stations yielded useful first-arrivals to source-receiver offsets beyond 10 km: the average maximum source-receiver offset for first arrivals was 17 km. Six stations yielded no useful data and useful first-arrivals were limited to offsets less than 10 km at five stations. We separately archived our recordings of 86 local and regional earthquakes ranging in magnitude from 0.2 to 4.3 and 16 teleseisms ranging in magnitude 5.5 to 6.5. CONTENTS Abstract 1 Introduction 3 Data Acquisition 3 CCGS Tully Instrumentation and Operations 3 Wide-Angle Recording 4 Reftek Instrumentation 4 Station Deployment/Data Acquisition 4 Station Locations and Elevations 5 Reftek Data Reduction 5 Common Receiver Gathers 5 Earthquakes 5 Notes on Data Reduction 5 SEGY Trace Format 6 Description of the Data 6 Data Quality 6 Data Availability 7 Acknowledgments 7 References Cited 8 APPENDICES Appendix 1. Abbreviated list of airgun shotpoint FFID numbers, shot times, and locations 10 Appendix 2. CCGS Tully Lines, Times, FFID numbers, and line locations 15 Appendix 3. Reftek receiver station locations and elevations, reoccupations of 1998 SHIPS sites, and estimates of signal propagation 19 Appendix 4. Statistics on GPS Reftek station locations and elevations 20 Appendix 5: Receiver DAS numbers, quality of timing, tape numbers, and comments 21 Appendix 6. PASSCAL SEGY trace header format 22 Appendix 7. Minimum receiver-source offsets (in meters) for each station for every Julian Day 23 Appendix 8. Local and Regional Earthquakes archived 24 Appendix 9. Teleseisms archived to tape. 25 FIGURES Figure 1. Map showing locations of seismic lines and recorders in the Georgia Strait 26 Figure 2. Record section for Reftek station 109 for CCGS Tully line 61 on JD 140 27 Figure 3. Record section for Reftek station 105 for CCGS Tully lines 33-34 on JD 137 28 Figure 4. Record section for Reftek station 113 for CCGS Tully line 10 on JD 135 29 Figure 5. Record section for Reftek station 151 for CCGS Tully line 9 on JD 135 30 Figure 6. Record section for Reftek station 160 for CCGS Tully line 3 on JD 135 31 Figure 7. Record section for Reftek station 128 for CCGS Tully line 56 on JD 139 32 Figure 8. Reftek recordings of earthquakenumber 300010 33 Figure 9. Reftek recordings of earthquake number 300064 33 INTRODUCTION In the past decade seismic hazards posed to northwestern Washington and southern British Columbia by crustal faulting have been recognized (e.g., Pratt et al., 1997; Cassidy et al., 2000; Mosher et al., 2000; Johnson et al., 2001). The existence of crustal faults capable of large (M~7) magnitude earthquakes within Puget Lowland has been inferred and mapped using a variety of methods including paleoseismic, seismicity, seismic reflection, and potential field geophysical data (Atwater and Moore, 1992; Bucknam et al., 1992; Johnson et al., 1994, 1996; Pratt et al., 1997; Wells et al., 1998; Blakely et al., 2002; ten Brink et al., 2002). In 1998 the Seismic Hazard Investigation in Puget Sound (SHIPS) surveyed the southern Georgia basin, yielding new crustal scale tomography velocity models for this important structure (Ramachandran, 2001; Zelt et al., 2001). Although the geology of the San Juan Islands and Lummi Peninsula have been reported (Vance, 1975, 1977; Brandon et al., 1988; Garver, 1988a,b; Droost, 1996), as well as that of the Georgia Basin (England and Bustin, 1998), few seismic studies of the Lummi Island and other crustal faults in the southern Georgia basin have been reported (Finkbeiner, 1994; Fisher et al., 2003). In this report we present wide-angle recordings obtained during a collaborative experiment between the Pacific Geoscience Centre (PGC), the U.S. Geological Survey (USGS), and the University of Victoria (Riedel, 2002; Riedel et al., 2002). The experiment, conducted using the Canadian Coast Guard Ship (CCGS) Tully and temporary deployments of land-based seismic recorders, was centered on the southern Georgia basin (Figure 1). The survey was designed to provide new wide-angle seismic profiles complimentary to SHIPS data and to image crustal faults. The cruise was divided into two parts, the first taking place mainly in U.S. waters (May 13-17) focusing on the Lummi Island fault and the southern extension of the Outer Island fault. The second part (May 17-May 26) was focused in Canadian waters on the location of frequent earthquake activity north-east of Gabriola Island, the northern extent of the Outer Island fault, and known recent Holocene faults in the vicinity of Vancouver, British Columbia. DATA ACQUISITION CCGS Tully Instrumentation and Operations In the middle of May, 2002, we acquired nearly 180 shallow penetration marine seismic-reflection profiles in the Strait of Georgia using the CCGS Tully (Figure 1). Shipboard operations were described in a cruise report by Riedel (2002). The CCGS Tully used a single 1.967 liter (120 cu. in.) airgun as the sound source, towed at a depth of about 4 meters, and operated at a nominal air pressure of 1900 psi. Airgun shots were fired at 5 second intervals to minimize the common-midpoint spacing of the MCS data. Airgun repetition rates ranged between 5.000 and 5.492 seconds; starting at 20:21 UTC on JD 138 and for most of the cruise they were 5.384 seconds. Signals from a blast phone (Bolt time-break solenoid valve model SV-1200-511) attached to the airgun power- and air-supply cables (Riedel, 2002) within meters of the CCGS Tully air gun were continuously recorded on a RefTek recorder connected to a Global Positioning System (GPS) clock. Air gun firing times were automatically picked from this record using the IRIS/PASSCAL software program reftrig. The resulting shot list was edited by hand to remove duplicate triggers. These air gun origin times are believed to be accurate to within one or two milliseconds. Navigation of the CCGS Tully was also achieved using a GPS receiver; these absolute coordinates are estimated to be accurate to within 40 m. The airgun shot locations presented here represent locations for the midpoint of the airgun having been corrected for the offset between the GPS antenna and the airgun. For the first three days of the experiment, Julian Day (JD) 135 to JD 137 (May 15th to 17th), the CCGS Tully collected 36 short lines near Lummi Island, the San Juan Islands, and the Outer Islands. From Julian Day 138 to 139 the Tully collected 20 lines in the Georgia Strait. Between Julian Day 139 and 141 the Tully collected 20 lines in the epicentral region of a 1997 earthquake (Cassidy et al., 2000). From Julian Day 141 to the end of the survey on Julian Day 146, the Tully collected 100 lines in a 5-km by 10-km 3-D seismic survey of a pockmark field thought to have formed along an active crustal fault. The airgun lines were spaced 50 m apart in the 3-D grid (Fig. 1). Figure 1 presents the CCGS Tully lines in map view. Appendix 1 provides an abbreviated list of the shot locations (northings, eastings, latitudes, and longitudes) and shot times for the entire CCGS Tully cruise given for shots acquired at hourly intervals. Appendix 2 provides start and end origin times and the beginning and ending FFIDs of the CCGS Tully seismic lines as numbered onboard the CCGS Tully. For our processing of the wide-angle Reftek data into common-receiver gathers we rearranged and reduced the number of airgun shotlines into 12 separate seismic lines, one for each Julian Day of the survey (Appendix 1). We renumbered the airgun shot Field File Identification Numbers (FFIDs) so that each airgun shot now has a unique FFID. Appendices 1 and 2 provide the FFIDs as they were written to archival tape. Wide-Angle Recording The signals generated by the air gun towed by the CCGS Tully were recorded in a wide-angle geometry using 48 Reftek recorders deployed onshore. Given the small volume of the CCGS Tully airgun, most of recorders were deployed along the Strait of Georgia within 10 km of the planned ship tracks (Figure 1). Thirteen of the sites used for RefTek stations represent reoccupations of 1998 SHIPS sites (Brocher et al., 1999) (Appendix 3). The other sites selected were chosen to increase the density of SHIPS wide-angle recordings to permit the inversion for higher-resolution tomography velocity models in the southern Georgia basin. 23 stations were deployed in the Outer Islands, 12 sites were deployed on Lummi Island, Lummi Peninsula, and Orcas Island, 7 stations were deployed on the Canadian mainland, and 6 sites were deployed on the U.S. mainland. Air gun signals were recorded at ranges as close as 1 km and as far as 120 km. Appendix 3 presents the RefTek DAS number, location (northings, eastings, latitudes, and longitudes), and elevation of each Reftek station. It provides the station number of the 1998 SHIPS site previously deployed at or near the station, if any. The digital Reftek recorders deployed consisted of five major components (PASSCAL, 1991). These components include the (1) Data Acquisition System (DAS), (2) internal or external hard disk drive, (3) internal oscillator and, in most cases, internal or external GPS Clock, (4) 3-component seismometer, and (5) external batteries. The GPS receiver clocks were typically recorded once per hour. Recording was simply halted when the instrument was retrieved. Reftek Instrumentation We recorded three-component data using three different RefTek models (models 06s, 07s, 07Gs). Reftek 06's have external GPS receiver and antennas. DAS serial numbers for Reftek 06s had four digits starting with a 6. The Reftek 07's have either internal or external GPS receivers and antennas. DAS serial numbers for Reftek 07s had four digits starting with a 7. The Reftek 07G's have internal GPS receivers and antennas The geophone sensors were Mark Products model L-28s, which are 4.5 Hz, 3-component seismometers. The sensors were oriented with compasses such that the N-S component was directed to magnetic north. Channel 1 recorded the vertical component, channel 2 recorded the N-S oriented horizontal component, and channel 3 recorded the E-W oriented horizontal component. Power needs of the Refteks required us to deploy two 12-V, 80-Amp/Hr car batteries connected in parallel at each site. To protect them from the elements, at each station the equipment was deployed in firm plastic enclosures (Action Packers). Station Deployment/Data Acquisition Almost all Reftek recorders were deployed over a two-day period from JD 131 to JD 133 (May 11 to 13th). The first airgun shots were fired at 0830 Universal Time (UTC) on JD 135 (May 15th). The last airgun shot was fired in the eastern Strait of Juan de Fuca at 2135 UTC on JD 146 (May 26th). Retrieval of the Refteks was completed on JD 147 (May 27th). Wide-angle recorders were deployed by two teams each from the University of Victoria (stations 101-130; Fig. 1) and the U.S. Geological Survey (stations 150-167; Fig. 1). Each team was responsible for deploying and maintaining between 10 and 14 stations. The DAS at one Reftek station, 122, deployed in British Columbia, was stolen. All Refteks were programmed to record the following parameters: (1) continuous recording with a sample rate of 100 Hz, (2) recording to start at the time of deployment, (3) recording to be halted at the time of retrieval, and (4) the continuously recorded data were divided into 60-minute-long events. Station Locations and Elevations The built-in or auxiliary GPS receiver at each station provided estimates of the station latitude, longitude, and elevation (Appendix 3). The GPS coordinates in Appendix 3 generally represent the average GPS location recorded once an hour (providing a median of 133 separate measurements). The median uncertainties (1 standard deviation from the average location) of the latitudes and longitudes are about 7 m (Appendix 4). The median uncertainty in elevation is 17 m (Appendix 4). To the elevations provided by these GPS receivers we added 19 m, the same correction applied by Brocher et al. (1999). REFTEK DATA REDUCTION Common receiver gathers Data were cut as 20-second-long traces starting at the shot time. The data are unreduced. All three components were cut and archived. Ref2segy was used to extract segy traces from the raw (.ref) files. Timing corrections were computed from the log files (.log) using the refrate program. DAS 7296 was moved on Julian Day 140-141, resulting in two log files and two pcf files; these two pcf files were concatenated to produce a single file for the timing corrections. The timing files (.pcf) were checked visually with the clockview program to see that timing corrections were properly handled. In the cases where timing errors were not properly handled, the pcf files were hand-edited to correct the problem. Appendix 5 lists the DASes and times where corrections were edited. Timing corrections were applied by the segycut program during the data cutting stage. The trace headers contain the station number, shot number, DAS number, source and receiver elevations (in meters), and UTM coordinates of the source and receiver (in meters). Data were written to DAT tapes as common-receiver gathers, with three gathers (three components) per day for each DAS. Earthquakes Eighty-six local earthquakes were saved as PASSCAL segy traces with a record length of 300 sec (5 minutes) starting 60 sec before the origin time of the earthquake (Appendix 8). Sixteen teleseisms were saved as PASSCAL segy traces with a record length of 3600 sec (1 hour) starting at the origin time of the earthquake (Appendix 9). The individual traces (3 components per DAS) are located in directories named for the start time of the traces (60 sec before the origin time). Timing corrections were applied to all traces before cutting the earthquakes as described for the processing of the common receiver gathers. Appendix 5 lists the DASes and times where corrections were hand edited. The pcf files were then concatenated into a single file, which was used as input to the clockcor program to adjust the timing. The records were then cut using the eqcut graphic interface to the segycut program. The headers of all traces in the earthquake data contain the receiver (station) number, receiver elevation in meters, and receiver latitude and longitude. The latitude and longitude are given as integer values, and need to be divided by 3600 to obtain decimal degrees. Notes: 1) A total of approximately 15 Gbytes of rawrefdump-formatted data were acquired. During the data reformatting data volumes were expanded by a factor of 4. Twenty-second records of unreduced data were archived for each airgun shot. 2) GPS locks recorded in the logfiles for each station were averaged to provide GPS estimates of the station location and elevation using the program position (Appendix 3). Statistics of these estimates are given in Appendix 4. 3) A file containing the receiver (station) number, DAS number, the receiver UTMs (in meters), decimal longitude and latitude, and receiver elevation (in meters) was compiled (Appendix 3). 4) The more than 160,300 airgun shots were divided into 12 separate shot files; one file for each Julian Day. SEGY Trace Format The common receiver gathers were written in an unreduced travel time format in industry-standard SEGY format. Twenty-seconds of data were saved for each trace, starting at the airgun origin time. At a sample rate of 10 ms, there are 2001 samples per trace, for a block length, including header, of 8244 bytes per trace (including the 240-byte SEGY trace header). The time interval between airgun shots is approximately 5 s. SEGY trace header formats are described by Barry et al. (1975) and in Appendix 6. The modification comes from the fact that we use some of the unspecified header words to store information pertinent to the PASSCAL data. The data values for each trace are preceded by a 240 byte header. The format of the header is given in Appendix 6. All integer values are stored with the most significant byte first. Data values are 32 bit, IEEE floating point numbers. Tape copies are available from the IRIS/PASSCAL Data Management Center. Earthquake data are written in PASSCAL SEGY format, which is a modified version of the SEGY format. In the PASSCAL format, each trace is a separate file, and the data are either 16-bit integers (06 DAS) or 32-bit integers (07 DAS). The trace header locations are shown in Appendix 6. In the earthquake data, the source location is not in the header, and the receiver location is given in latitude and longitude (decimal degrees times 3600). DESCRIPTION OF THE DATA The data show several seismic arrivals. First arrivals consisting of direct arrivals and refractions from the sedimentary basin fill were well recorded (e.g., Figs. 2 to 7). Strong secondary arrivals were routinely recorded (Figs. 2, 3, and 7). Water waves are also commonly observed (e.g., Figs. 2 and 5). Examples of local earthquakes recorded during our two-week deployment are shown in Figures 8 and 9. In these plots, the traces are ordered from nearest to farthest from the earthquake epicenter, and traces from all three components are plotted. DATA QUALITY Useful first arrivals were recorded at 42 of the 48 stations. Examples of the common-receiver gathers that we obtained are provided in Figures 2 to 7. First arrivals are typically low frequency, approximately 10 Hz. The 5-second airgun repetition rate causes a great deal of sound to be in the water column on these records (e.g., Fig. 2), particularly at the smallest source-receiver separations (less than 10 km). In addition, very strong secondary arrivals, possibly shear-waves, interfere with the first arrivals when source-receiver offsets are small (e.g., Figs. 3 and 5). In some cases, these secondary arrivals can be traced to greater offsets than the first arrivals (e.g., Fig. 6). Appendix 3 presents an estimate to the maximum range that useful first-arrivals can be observed for each RefTek station, for the Julian Day of the closest approach of the Tully to the receiver. For the 46 stations that yielded data, the average maximum range for which useful first arrivals could be observed was 17 km. Thirty-seven out of 48 stations (77%) provided usable first arrival data to source-receiver offsets of at least 10 km (Appendix 3). First arrivals could be traced to offsets less than 10 km for only 5 stations (Appendix 3). 17 stations recorded useful first arrivals to offsets between 10 and 20 km (Appendix 3). First arrivals were observed to offsets of or beyond 20 km for 20 stations (Appendix 3). No first arrivals were observed in data from stations near urban centers on the mainland in Canadian and U.S. (stations 125, 126, 156, and 157). No data were recorded at Stations 119 and 122. Eleven local earthquakes occurring within the map area of Figure 1 were recorded by our RefTek array (Appendix 8). The largest of these events, 300010, had a magnitude of 2.7 and originated 44 km below Victoria. Because it occurred early in our deployment, it was recorded by 25 stations at the southern end of our RefTek array (Fig. 8). Event 300047 also had a magnitude of 2.7 and originated just SE of Figure 1. It was recorded by 37 of our stations (Fig. 9). The remaining 10 local events had magnitudes ranging from 0.2 to 1.8. The magnitudes of the 16 teleseisms that we recorded ranged from 5.5 to 6.5. Only three teleseisms had magnitudes greater than 6.0 (Appendix 9). None of these teleseisms were obvious on records filtered with a low-frequency bandpass. The largest teleseism, 400016, had a magnitude of 6.5, occurred at a depth of 109 km just north of the Banda Sea (Appendix 9). This teleseism occurred in the later stages of our recording interval, and as consequence was recorded only by 17 stations at the northern end of our deployment. Favorable weather conditions were encountered, and this favorable weather undoubtedly contributed to the data quality. There were few extended periods of high winds during the experiment. DATA AVAILABILITY Copies of the SEGY common receiver gathers may be ordered via email from the IRIS/PASSCAL Data Management Center (DMC) in Seattle, Washington. The current email address of the Incorporated Research Institutions for Seismology (IRIS) Consortium is: www.iris.edu. The current general email address for the IRIS DMC is webmaster@iris.washington.edu. The current address of the IRIS DMC is: 1408 NE 45th St., Suite 201, Seattle, WA 98105. telephone (206) 547-0393. Tim Ahern is currently the Program Manger of the IRIS Data Management System at Seattle. ACKNOWLEDGMENTS This field work was supported by the Pacific Geoscience Centre of the Geological Survey of Canada. Salary support was provided by the U.S. Geological Survey. In Washington state, Elizabeth Barnett and Lynn Hultgrien, USGS, and Willy Lynch, a USGS volunteer, organized and arranged permits for the field work. Elizabeth Barnett, Willy Lynch, and Lynn Hultgrien deployed and retrieved the RefTek stations in the U.S. In British Columbia, Ivana Novosel, Caleb Fort, Johanna Hoehne, Richard Fitton, Mikhail Zykov, Lidia Zykov (UVic), and David Mate (PGC) deployed and retrieved the RefTek stations. The IRIS/PASSCAL Instrument Facility loaned the RefTeks used to record the airgun shots. Mike Fort of IRIS/PASSCAL prepared the RefTek instruments for deployment in Canada. Russell Sell made cables allowing us to record the airgun blast phone signal on a RefTek recorder, and generated the airgun shottime list using PASSCAL software. TheWashington State Departments of Forestry and Parks and Recreation granted permission to access land under their jurisdiction. Numerous property owners granted permission to access their land. The Lummi Indian Nation (Leroy Deardorff) and the Lyaeksun First Nation (Rick Thomas, Chief; Barbara Thomas, band administrator) granted access to their land. The National Marine Fisheries Service (NMFS) granted a permit to allow airgun profiling in U.S. waters. Ken Hollingshead of NMFS was especially helpful during the marine mammal permitting process. John Calambokidis, Annie Douglas, Lisa Schlender, Nora Moloney, Suzanne Stircker, and Cody Massing of Cascadia Research, and Jennifer Balke, provided marine mammal observations. We thank the CCGS Tully science party, the captain, and ships crew. Shirley Baher, USGS, critically reviewed this report. REFERENCES CITED Atwater, B.F., and Moore, A.L., 1992, A tsunami about 1000 years ago in Puget Sound, Washington, Science, v. 258, p. 16141617. Barry, K.M., D.A. Cravers, and C.W. Kneale, 1975, Recommended standards for digital tape formats: Geophysics, v. 40, p. 344-352. Blakely, R.J., Wells, R.E., Weaver, C.S., and Johnson, S.Y., 2002, Location, structure, and seismicity of the Seattle fault, Washington: Evidence from aeromagnetic anomalies, geologic mapping, and seismic-reflection data, Geological Society of America Bulletin, 114, 169-177. Brandon, M.T., Cowan, D.S. and Vance, J.A., 1988, The Late Cretaceous San Juan thrust system, San Juan Islands, Washington, Geological Society of America, Special Paper 221, 81 pp. Brocher, T.M., T. Parsons, R.A. Blakely, N.I. Christensen, M.A. Fisher, R.E. Wells, and the SHIPS Working Group, 2001, Upper crustal structure in Puget Lowland, Washington: Results from 1998 Seismic Hazards Investigation in Puget Sound, J. Geophy. Res., 106, 13,541-13,564. Brocher, T.M., T. Parsons, K. C. Creager, R. S. Crosson, N. P. Symons, G. Spence, B.C. Zelt, P.T.C. Hammer, R. D. Hyndman, A. M. Trhu, K. C. Miller, U.S. ten Brink, M.A. Fisher, T. L. Pratt, M.G. Alvarez, and B.C. Beaudoin, 1999, Wide-angle seismic recordings from the 1998 Seismic Hazards Investigation in Puget Sound (SHIPS), western Washington and British Columbia, U.S. Geological Survey Open-File Report 99-314, 110 p. Bucknam, R.C., HemphillHaley, E., and Leopold, E.B., 1992, Abrupt uplift within the past 1700 years at southern Puget Sound, Washington, Science, v. 258, p. 16111614. Cassidy, J.F., G. C. Rogers, and F. Waldhauser, 2000, Characterization of active faulting beneath the Strait of Georgia, British Columbia, Bull. Seismol. Soc. Amer., 90, 1188-1199. Drost, B.W., 1996, Selected ground-water data for the Lummi Indian Reservation, Whatcom County, Washington, U. S. Geological Survey Open File Report 96-0166, 21 pp., 1 sheet. England, T.D.J., and R.M. Bustin, Architecture of the Georgia Basin, southwestern British Columbia, Bull. Can. Petrol. Geology, 46, 288-320, 1998. Finkbeiner, T., 1994, Tectonic and sedimentary basins in the Pacific Northwest, M.S. thesis, Stanford University, Palo Alto, 80 pp. Fisher, M.A., R.D. Hyndman, S.Y. Johnson, R.S. Crosson, U.S. ten Brink, A.J. Calvert, T.M. Brocher, R.E. Wells, and the SHIPS Working Group, 2003, Crustal structure and earthquake hazards of the Subduction Zone in the Central Part of Cascadia, U.S. Geological Survey Professional Paper. Garver, J., 1988a, Stratigraphy, depositional setting, and tectonic significance of the clastic cover to the Fidalgo Ophiolite, San Juan Islands, Washington, Canadian Journal of Earth Sciences, v. 25, no. 3, pp. 417-432. Garver, J.I., 1988b, Fragment of the Coast Range Ophiolite and the Great Valley Sequence in the San Juan Islands, Washington, Geology, v. 16, no. 10, pp. 948-951. Johnson, S.Y., Potter, C.J., and Armentrout, J.M., 1994, Origin and evolution of the Seattle fault and Seattle basin, Washington, Geology, v. 22, p. 7174. Johnson, S.Y., Potter, C.J., Armentrout, J.M., Miller, J.J., Finn, C., and Weaver, C.S., 1996, The southern Whidbey Island fault, western Washington-An active structure in the Puget Lowland, Washington: Geological Society of America Bulletin, v. 108, p. 334-354, and oversized insert. Johnson, S.Y., Dadsman, S.V., Mosher, D.C., Blakely, R.J., and Childs, J.R., 2001, Active tectonics of the Devils Mountain fault and related structures, northern Puget Lowland and eastern Strait of Juan de Fuca region, Pacific Northwest, U.S. Geological Survey Professional Paper 1643 (65 p. text, 2 tables, 38 figs., 2 plates). Mosher, D.C., J.F. Cassidy, C. Lowe, Y. Mi, R.D. Hyndman, G.C. Rogers, and M. Fisher, 2000, Neotectonics in the Strait of Georgia: First tentative correlation of seismicity with shallow geological structure in southwestern British Columbia, Geol. Survey of Canada, Current Research 2000-A22, 9 p. PASSCAL, 1991, Users Guide, A Guide to Planning Experiments Using PASSCAL Instruments: IRIS, 28 pp. Pratt, T.L., S. Johnson, C. Potter, W. Stephenson, and C. Finn, 1997, Seismic reflection images beneath Puget Sound, western Washington state: The Puget Lowland thrust sheet hypothesis, J. Geophys. Res., 102, 27,469-27,489. Riedel, M., 2002, Georgia Basin Geohazards Initiative mapping of near surface active faults, Report on Cruise PGC02002 on C.G.G. J.P Tully, Pacific Geoscience Centre, Sydney, B.C., 118 p. Riedel, M., V. Barrie, P. Hill, T.M. Brocher, T.L. Pratt, and R.D. Hyndman, 2002, Mapping of near surface active faults in Georgia basin, Eos Trans. AGU, 83(47), Fall Meet. Suppl., Abstract S22B-1031. ten Brink U. S., P.C. Molzer, M.A. Fisher, R.J. Blakely, R.C. Bucknam, T. Parsons, R.S. Crosson and K.C. Creager, 2002, Subsurface geometry and evolution of the Seattle fault zone and the Seattle basin, Washington, Bull. Seism. Soc. Am., 92, 1737-1753. Vance, J.A., 1975, Bedrock geology of San Juan County; Geology and water resources of the San Juan Islands, San Juan County, Washington Water-Supply Bulletin, Washington State Department of Ecology, no. 46, pp. 3-19. Vance, J.A., 1977, The stratigraphy and structure of Orcas Island, San Juan Islands, Geological excursions in the Pacific Northwest, Editor, Brown, E H; Ellis, R C., Geol. Soc. Am., Boulder, Colo., p. 170-203. Wells, R.E., Weaver, C.S., and Blakely, R.J., 1998, Fore-arc migration in Cascadia and its neotectonic significance, Geology, 26, 759-762. Appendix 1. Abbreviated list of airgun shotpoint FFID numbers, shot times, and locations FFID Year JD Hr Mn SecondEasting, mNorthing, mDepth, mLatitude NAD 83Longitude NAD 83110175200213582553.5985178895382931-448.5992-122.757411057520021351002.0825240185389497-448.6581-122.673911129520021351101.1105298605382241-448.5925-122.595011198320021351200.1385285845391179-448.6730-122.611711270420021351304.1585228565399928-448.7519-122.689111342420021351403.1845180415404943-448.7972-122.754311414420021351502.2105157785395352-448.7110-122.785511486420021351601.2385090845396196-448.7187-122.876511554720021351700.2745108695402445-448.7749-122.852111618820021351804.5065079335406771-448.8139-122.891911684320021351902.4425025255412586-448.8662-122.965611748920021352000.3604981705418223-448.9169-123.025011810320021352103.7924925405424488-448.9733-123.1019118623200213522010.5124887015417630-448.9115-123.154211913720021352302.9364843545411287-448.8543-123.21331197792002136000.8604825315418431-448.9186-123.23841203962002136104.2804871695425417-448.9815-123.1754120571200213611839.3624885335424649-448.9746-123.1567120618200213671351.3925152595404455-448.7929-122.79221211452002136803.2245170535398694-448.7410-122.76811218652002136902.2485213295390786-448.6698-122.710312258520021361001.2725287475386792-448.6335-122.609812330520021361100.2965217985392420-448.6844-122.703812402620021361204.3205171235399761-448.7506-122.767112474620021361303.3465131765408652-448.8307-122.820512546620021361402.3705074825416392-448.9004-122.897912618620021361501.3964989145412607-448.8664-123.014812684320021361602.9744935965407140-448.8172-123.087212749720021361700.9004940845413160-448.8714-123.080712815320021361804.3184985945419452-448.9280-123.019212880820021361902.2445005395408707-448.8313-122.992712946320021362000.1705013185397726-448.7326-122.982113011920021362103.5904960185389259-448.6564-123.054113077420021362201.5164885465394382-448.7024-123.155713143020021362304.9364955225400388-448.7565-123.06091320852002137002.8625026035406905-448.8151-122.96451327402002137100.7905079925413362-448.8732-122.89101333962002137204.2105136345409861-448.8416-122.81421340512002137302.1365056315415082-448.8887-122.92321347062002137400.0624978135418472-448.9192-123.02991353622002137503.4824900105422923-448.9591-123.13651360172002137601.4104822885427818-449.0030-123.24221366732002137704.8284769375423140-448.9607-123.31511373282002137802.7564852075419200-448.9256-123.20201379832002137900.6824930605413728-448.8765-123.094613863920021371004.1005007535408345-448.8281-122.989713929420021371102.0265096005402917-448.7792-122.869313995020021371205.4465168695397695-448.7320-122.770614060520021371303.3725219905390986-448.6715-122.701314126020021371401.2985177835399566-448.7489-122.758114191620021371504.7185093585405410-448.8016-122.87261423432002137153910.2365068815407763-448.8228-122.90621423442002137163528.4425028965406178-448.8086-122.960614259620021371700.5744997115403589-448.7853-123.003914324820021371803.9884895415399747-448.7506-123.142314390320021371901.9164883675400022-448.7531-123.158314455920021372005.3344797845398021-448.7349-123.274914521420021372103.2604751785402135-448.7717-123.337814586920021372201.1884746845409106-448.8344-123.345014652420021372304.6084673145414837-448.8856-123.44591471792002138002.5344608635421392-448.9442-123.53451478342002138100.4604552905428459-449.0074-123.61141484902002138203.8804479745432938-449.0471-123.71201491452002138301.8064464275426439-448.9885-123.7323149482200213833052.9544482085422958-448.9574-123.7075149483200213874138.3304773785421945-448.9500-123.30901496842002138802.4264767665424319-448.9713-123.31751503002002138900.3504732305419848-448.9310-123.365515094620021389598.8404753135425340-448.9805-123.33741509472002138122237.0244708445427658-449.0011-123.398615124220021381304.7464696975429152-449.0145-123.414415189720021381402.6724648065425753-448.9837-123.481015255120021381500.5984703425432135-449.0414-123.405815320720021381604.0164654525428764-449.0108-123.472415386220021381701.9424643755430290-449.0245-123.487315442020021381805.3604678265433201-449.0508-123.440315507520021381903.2884633845432531-449.0446-123.501115573020021382001.2124609565432889-449.0476-123.534315635220021382100.4044668475438072-449.0946-123.454115702120021382201.7364665965440731-449.1185-123.457815769020021382303.0684603615435866-449.0744-123.54271583592002139004.4004587015436844-449.0831-123.56561589822002139100.3484670625441912-449.1292-123.45151596492002139201.6824700015446350-449.1692-123.41151603152002139303.0244658815445358-449.1601-123.46801609832002139404.3504569345441447-449.1243-123.59031616452002139500.2944595285444778-449.1545-123.55501623142002139601.6264683785448861-449.1917-123.43401629662002139702.9624714085453216-449.2311-123.39271636352002139804.2924664185450313-449.2047-123.46101642932002139900.2424578945446497-449.1698-123.577616495920021391001.5744550785451548-449.2151-123.616816562820021391102.9084551315459483-449.2864-123.617016629720021391204.2384522215465019-449.3360-123.657716696520021391300.1884514915455929-449.2542-123.666616763420021391401.5204515535446367-449.1682-123.664616812320021391502.8524562825450079-449.2019-123.600116879220021391604.1824563565459270-449.2846-123.600116946020021391700.1304550185464699-449.3334-123.619117012920021391801.4604527175457012-449.2640-123.649917079820021391902.7944526295446944-449.1735-123.64991709612002139191440.2464536725445425-449.1599-123.635417096220021401659.8964510105446078-449.1656-123.67201715532002140201.3464502385451308-449.2125-123.68331722222002140302.6784502515460734-449.2973-123.68421728912002140404.0104539415463204-449.3198-123.63381735602002140505.3424539135455201-449.2478-123.63321742282002140601.2904538595446748-449.1718-123.63301748972002140702.6224574975450423-449.2051-123.58351755662002140803.9564575705459987-449.2912-123.58351762352002140905.2864587225457388-449.2679-123.567417690320021401001.2384586795448748-449.1901-123.567117757220021401102.5684599255451105-449.2114-123.550217824120021401203.9004599905459435-449.2864-123.550217891020021401305.2344611845461568-449.3056-123.534017957820021401401.1824611575453667-449.2346-123.533618024720021401502.5144605395446803-449.1728-123.54141803742002140151126.1764602855448042-449.1839-123.5450180375200214022334.4724614785444488-449.1520-123.528318101020021402300.4784623485452232-449.2217-123.51711816792002141001.8104627515461382-449.3040-123.51241823482002141103.1384635845453940-449.2371-123.50031830172002141204.4724589755449861-449.2002-123.56311836852002141300.4204515295451643-449.2157-123.66561843542002141401.7544607785451736-449.2172-123.53861850232002141503.0864625755453516-449.2333-123.51411856922002141604.4164527445453641-449.2337-123.64911863602002141700.3684570345455426-449.2501-123.59041870292002141801.7004650365455391-449.2503-123.48041876982002141903.0324635895457250-449.2669-123.500518836720021411004.3644551815457306-449.2669-123.616118903520021411100.3124532535459193-449.2837-123.642819037320021411302.9764648005451180-449.2124-123.483319104220021411404.3084642095451397-449.2143-123.491419171020021411500.2544677245454485-449.2423-123.443419237920021411601.5864631825449174-449.1943-123.505319304820021411702.9204678655456190-449.2576-123.441619371720021411804.2544646175449289-449.1954-123.485619438520021411900.2024666935455303-449.2496-123.4577194497200214119103.1124673695456555-449.2609-123.44851944982002141212311.7164677525456081-449.2566-123.443219490920021412204.1944661405451710-449.2172-123.46501953662002141224825.7224640535450888-449.2097-123.49351961642002142001.4824674095453702-449.2352-123.44771968332002142102.8144635125449908-449.2009-123.50091975022002142204.1464686355455654-449.2528-123.43101981702002142300.0924640325448339-449.1868-123.49361988392002142401.4284673215456066-449.2565-123.44911995082002142502.7584652495449984-449.2017-123.47702001772002142604.0924661475454086-449.2386-123.46512008452002142700.0424661745451388-449.2143-123.46452015142002142801.3724624475445423-449.1605-123.51512021832002142902.7024648155448036-449.1841-123.482820285220021421004.0344660875453860-449.2366-123.465920352120021421105.3684661205451255-449.2131-123.465220418920021421201.3164651995452300-449.2225-123.477920485820021421302.6484669275452499-449.2244-123.454220552720021421403.9784642475450679-449.2079-123.490920619620021421505.3084680825454266-449.2403-123.438520686420021421601.2564635985449453-449.1968-123.499620753320021421702.5864685075454925-449.2463-123.432720820220021421803.9184635115448988-449.1926-123.500820887120021421905.2484686455455724-449.2535-123.430920953920021422001.2004648095448719-449.1903-123.483021005120021422102.5344596015442657-449.1354-123.553821072020021422203.8664626645447678-449.1808-123.512321138920021422305.1984674065455588-449.2522-123.44792120392002143001.1444654135449652-449.1987-123.47482127082002143102.4804666795454295-449.2405-123.45782133772002143203.8124661135450685-449.2080-123.46522140462002143305.1444660625453211-449.2307-123.46622146182002143401.0924671975452373-449.2233-123.45052152872002143502.4264644395450441-449.2057-123.48822159562002143603.7564682235453982-449.2378-123.43652166252002143705.0884637915449296-449.1954-123.49702172902002143801.0364694625455521-449.2517-123.41962179592002143902.3724688205453229-449.2310-123.428321862820021431003.7044691625454860-449.2457-123.423721929720021431105.0344649165448463-449.1880-123.481521996520021431200.9844672355454846-449.2455-123.450222063420021431302.3144649775448467-449.1880-123.480622130520021431403.6444671315454596-449.2433-123.451622197520021431504.9784658365449782-449.1999-123.469022253120021431600.9284668555454047-449.2383-123.455322320020021431702.2604662675450406-449.2055-123.463122386920021431803.5924666895453706-449.2352-123.457622453820021431904.9264663725450486-449.2062-123.461722520620021432000.8724665655453408-449.2325-123.459322587520021432102.2044669315451311-449.2137-123.454122654420021432203.5344656225451773-449.2178-123.472122721220021432304.8684678465452736-449.2266-123.44162278802002144000.8184647385450243-449.2040-123.48412285492002144102.1484688865454373-449.2413-123.42752292182002144203.4804637545448571-449.1889-123.49742298872002144304.8124687345455748-449.2537-123.42962305552002144400.7604651485448150-449.1852-123.47832312242002144502.0924676715454851-449.2456-123.44422318932002144603.4264660755449540-449.1977-123.46572325622002144704.7564670525453743-449.2356-123.45262332302002144800.7044668245450705-449.2082-123.45552338992002144902.0384664435452683-449.2260-123.460923456820021441003.3684667965450557-449.2069-123.455923523720021441104.7024664585452588-449.2252-123.460723590520021441200.6504669925450803-449.2091-123.453223657420021441301.9804668135453098-449.2298-123.455823724320021441403.3084667905450378-449.2053-123.455923791120021441504.6444656345452508-449.2244-123.472023857920021441600.5944662285453023-449.2291-123.463923924820021441701.9184647045451949-449.2193-123.484723991720021441803.2504659905452809-449.2271-123.467124058620021441904.5824645715450579-449.2070-123.486424125420021442000.5384670845454079-449.2386-123.452224190020021442101.8644679925455649-449.2528-123.43982424422002144214839.5424669245451184-449.2125-123.454224244320021450614.3324672375454233-449.2400-123.45012430432002145104.2304676425449904-449.2011-123.44422437112002145200.1784679185452126-449.2211-123.44062443802002145301.5104678795450217-449.2039-123.44102450492002145402.8424679055452046-449.2204-123.44082457182002145504.1744678685450076-449.2026-123.44112463862002145600.1224674085451147-449.2122-123.44752470552002145701.4544689855451818-449.2184-123.42592477242002145802.7864664655449491-449.1973-123.46032483932002145904.1184697215452981-449.2289-123.415924916220021451101.3984698395454923-449.2463-123.414424983120021451202.7304662825447239-449.1770-123.462625050020021451304.0624697595454635-449.2437-123.415525116820021451400.0104664985447569-449.1800-123.459725183720021451501.3424694115454067-449.2386-123.420225250620021451602.6744664515447425-449.1787-123.460325317520021451704.0064695445454193-449.2397-123.418425384420021451805.3384668595447992-449.1838-123.454825451220021451901.2864694785454020-449.2382-123.419325518120021452002.6184675435449037-449.1933-123.445525585020021452103.9504685535452293-449.2226-123.431925651920021452205.2824683965450368-449.2053-123.433925718720021452301.2324676995450947-449.2105-123.44352578562002146002.5644691185451435-449.2149-123.42402585252002146103.8964671565449903-449.2010-123.45092591942002146205.2284695215452017-449.2202-123.41862598622002146301.1784651915446547-449.1707-123.47752605312002146402.5104700225454496-449.2425-123.41192612002002146503.8424667415447342-449.1780-123.45632618692002146605.1744695315453670-449.2350-123.41852625372002146701.1224686445450404-449.2056-123.43052632062002146802.4544682175451402-449.2146-123.43642638752002146903.7864685595450153-449.2034-123.431626454420021461005.1184681505451207-449.2128-123.437326520120021461101.0684685155449991-449.2019-123.432226587020021461202.4004690765452611-449.2255-123.424726653920021461303.7324676825448521-449.1886-123.443526720820021461405.0644687885452076-449.2207-123.428626787620021461501.0124683845449595-449.1983-123.434026854520021461602.3444684465451421-449.2148-123.433326921420021461703.6764686155449846-449.2006-123.430826988320021461805.0084671755449216-449.1949-123.450527055120021461900.9564712485452367-449.2234-123.394927122020021462002.2884660165454717-449.2443-123.466927188920021462103.6204675905448218-449.1859-123.44482720062002146211033.4504668535447072-449.1756-123.4548 Appendix 2. R/V Tully Lines, Times, RefTek FFID numbers, and line locations TullyStartUTCEndUTCStartEndNo. of Line No.JDHrMinJDHrMinFFIDFFIDShotsLocation11358:251359:47110175110430256Lummi/San Juan/Outer Isl.21359:4813511:06110431111386956Lummi/San Juan/Outer Isl.313511:0613513:481113871132881902Lummi/San Juan/Outer Isl.413513:4813515:121132891142901002Lummi/San Juan/Outer Isl.513515:1213516:03114291114906616Lummi/San Juan/Outer Isl.613516:0313517:05114907115596690Lummi/San Juan/Outer Isl.713517:0513521:091155971181712575Lummi/San Juan/Outer Isl.813521:0913522:51118172119035864Lummi/San Juan/Outer Isl.913522:5113523:32119036119478443Lummi/San Juan/Outer Isl.1013523:321361:181194791205711093Lummi/San Juan/Outer Isl.111367:131368:461206181216971080Lummi/San Juan/Outer Isl.121368:461369:58121698122569872Lummi/San Juan/Outer Isl.131369:5813614:041225701255142945Lummi/San Juan/Outer Isl.1413614:0413614:44125515125994480Lummi/San Juan/Outer Isl.1513614:4413615:38125995126610616Lummi/San Juan/Outer Isl.1613615:3813616:12126611126973363Lummi/San Juan/Outer Isl.1713616:1213617:561269741281431170Lummi/San Juan/Outer Isl.1813617:5613619:24128144129070927Lummi/San Juan/Outer Isl.1913619:2413620:16129071129658588Lummi/San Juan/Outer Isl.2013620:1613620:52129659130031373Lummi/San Juan/Outer Isl.2113620:5213621:51130032130682651Lummi/San Juan/Outer Isl.2213621:511370:591306831327292047Lummi/San Juan/Outer Isl.231370:591372:12132730133535806Lummi/San Juan/Outer Isl.241372:121376:011335361360272492Lummi/San Juan/Outer Isl.25a1376:011376:34136028136394367Lummi/San Juan/Outer Isl.25b1376:341376:53136395136596202Lummi/San Juan/Outer Isl.261376:5313712:561365971405613965Lummi/San Juan/Outer Isl.2713712:5613715:391405621423431782Lummi/San Juan/Outer Isl.2813716:3513717:49142344143129786Gulf Islands2913717:4913718:43143130143717588Gulf Islands3013718:4313719:03143718143936219Gulf Islands3113719:0313719:52143937144471535Gulf Islands3213719:5213720:45144472145050579Gulf Islands3313720:4513721:54145051145804754Gulf Islands3413721:541382:111458051486112807Gulf Islands351382:111383:30148612149482871Gulf Islands361387:411389:201494831505191037Georgia Strait371389:201389:59150528150946419Georgia Strait3813810:3713811:31---Georgia Strait3913811:3113811:43---Georgia Strait4013812:2213812:221509471509482Georgia Strait4113812:3313812:47150949151071123Georgia Strait4213812:4713813:48151072151766695Georgia Strait4313813:4813813:5415176715183165Georgia Strait4413813:5413815:13151832152694863Georgia Strait45a13815:1313815:1715269515273743Georgia Strait45b13815:1713816:24152738153469732Georgia Strait4613816:2413817:34153470154239770Georgia Strait4713817:4313818:32154240154770531Georgia Strait4813818:3213821:151547711565251755Georgia Strait4913821:4313823:271568321581251294Georgia Strait5013823:2713823:39158008158125118Georgia Strait5113823:391391:331581261593601235Georgia Strait521391:331392:17159361159840480Georgia Strait531392:171394:161598411611571317Georgia Strait541394:161396:241611581628761719Georgia Strait551396:241399:211628771645271651Georgia Strait561399:2113911:481645281661731646Earthquake Epi. N-S line.5713911:4813914:051661741676901517Earthquake Epi. N-S line.5813914:0513914:18167691167835145Earthquake Epi. N-S line.5913914:3513916:571678361694291594Earthquake Epi. N-S line.6013916:5713919:141694301709611532Earthquake Epi. N-S line.611401:061403:401709621726701709Earthquake Epi. N-S line.621403:401406:131726711743811711Earthquake Epi. N-S line.631406:131408:251743821758501469Earthquake Epi. N-S line.641408:2514010:191758511771221272Earthquake Epi. N-S line.6514010:1914012:401771231786931571Earthquake Epi. N-S line.6614012:4014015:001786941802521559Earthquake Epi. N-S line.66b14015:0014015:11180253180374122Earthquake Epi. N-S line.6714022:031410:091803751817811407Earthquake Epi. N-S line.681410:091411:27181782182649868Earthquake Epi. E-W line.691411:271412:50182650183575926Earthquake Epi. E-W line.701412:501414:391835761847891214Earthquake Epi. E-W line.711414:391416:07184790185776987Earthquake Epi. E-W line.721416:071418:371857771874441668Earthquake Epi. E-W line.731418:3714110:321874451887321288Earthquake Epi. E-W line.7414110:3214112:091887331898111079Earthquake Epi. E-W line.7514112:0914113:401898121908211010Earthquake Epi. E-W line.3D-0114113:4014114:45190822191545724Pockmark field. 3D-3114114:4514116:01191546192391846Pockmark field. 3D-0214116:0114117:04192392193098707Pockmark field. 3D-3214117:0414118:13193099193866768Pockmark field. 3D-0314118:1314119:10193867194497631Pockmark field. 3D-3314121:2314122:34194498195298801Pockmark field. 3D-04a14122:3414122:4819529919536668Pockmark field. 3D-04b14122:3914123:26---Pockmark field. 3D-3414123:591420:54196162196766605Pockmark field. 3D-051420:541421:59196767197500734Pockmark field. 3D-351421:591423:10197501198284784Pockmark field. 3D-061423:101424:12198285198975691Pockmark field. 3D-361424:121425:22198976199755780Pockmark field. 3D-071425:221426:25199756200459704Pockmark field. 3D-371426:251428:202004602017381279Pockmark field. 3D-081428:2014210:252017392031331395Pockmark field. 3D-3814210:2514211:34203134203905772Pockmark field. 3D-0914211:3414212:35203906204587682Pockmark field. 3D-3914212:3514213:45204588205363776Pockmark field. 3D-1014213:4514214:48205364206067704Pockmark field. 3D-4014214:4814215:54206068206804737Pockmark field. 3D-1114215:5414216:57206805207500696Pockmark field. 3D-4114216:5714217:57207501208173673Pockmark field. 3D-1214217:5714219:01208174208890717Pockmark field. 3D-4214219:0114220:592088912100411151Pockmark field. 3D-1314220:5914223:122100422115291488Pockmark field. 3D-4314223:121430:19211530212259730Pockmark field. 3D-141430:191431:23212260212972713Pockmark field. 3D-441431:231432:28212973213695723Pockmark field. 3D-151432:281433:01213696214064369Pockmark field. 3D-451433:101434:462140652151311067Pockmark field. 3D-161434:461435:50215132215845714Pockmark field. 3D-461435:501436:56215846216587742Pockmark field. 3D-171436:561437:55216588217239652Pockmark field. X-11437:551439:23217240218219980Pockmark field. 3D-471439:2314311:112182202194261207Pockmark field. 3D-1814311:1114312:13219427220116690Pockmark field. 3D-4814312:1314313:12220117220777661Pockmark field. 3D-1914313:1214314:20220778221533756Pockmark field. 3D-4914314:2014315:20221534222197664Pockmark field. 3D-2014315:2014316:23222198222791594Pockmark field. 3D-50a14316:2314316:2822279222284251Pockmark field. 3D-50b14316:2814317:24222843223467625Pockmark field. 3D-2114317:2414318:22223468224124657Pockmark field. 3D-5114318:2214319:28224125224853729Pockmark field. 3D-2214319:2814320:27224854225513660Pockmark field. 3D-5214320:2714321:34225514226264751Pockmark field. 3D-2314321:3414322:42226265227020756Pockmark field. 3D-5314322:4214323:45227021227722702Pockmark field. 3D-2414323:451440:54227723228482760Pockmark field. 3D-541440:541442:00228483229215733Pockmark field. 3D-251442:001443:06229216229955740Pockmark field. 3D-551443:061444:13229956230706751Pockmark field. 3D-261444:131445:15230707231394688Pockmark field. 3D-561445:151446:24231395232161767Pockmark field. 3D-271446:241447:22232162232813652Pockmark field. 3D-571447:221448:30232814233569756Pockmark field. 3D-281448:301449:28233570234219650Pockmark field. 3D-58a1449:2814410:29234220234893674Pockmark field. 3d-58b14410:1014410:16---Pockmark field. 3D-2914410:2914411:31234894235589696Pockmark field. 3D-5914411:3114412:28235590236226637Pockmark field. 3D-3014412:2814413:26236227236873647Pockmark field. 3D-6014413:2614414:33236874237613740Pockmark field. 3D-15r14414:3314415:34237614238289676Pockmark field. 3D-20r14415:3414416:37238290239002713Pockmark field. 3D-4r14416:3714417:36239003239649647Pockmark field. 3D-18r14417:3614418:41239650240376727Pockmark field. 3D-17r14418:4114419:44240377241075699Pockmark field. 3D-24r14419:4414420:30241076241587512Pockmark field. 3d-23r14420:3014421:14241588242056469Pockmark field. 3D-54r14421:1414421:48242057242442386Pockmark field. H-0914422:1614422:45---Extra Huntec Line H-1014422:4514423:35---Extra Huntec Line 3D-811450:061451:28242443243355913Pockmark field. 3D-611451:281452:27243356244017662Pockmark field. 3D-821452:271453:29244018244710693Pockmark field. 3D-621453:291454:28244711245362652Pockmark field. 3D-831454:281455:32245363246081719Pockmark field. 3D-631455:321456:37246082246806725Pockmark field. 3D-841456:371457:46246807247568762Pockmark field. 3D-641457:461458:46247569248245677Pockmark field. 3D-851458:461459:17248246248581336Pockmark field. 3D-6514510:0814511:06248582249236655Pockmark field. 3D-85r14511:0614512:06249237249907671Pockmark field. 3D-6614512:0614513:09249908250600693Pockmark field. 3D-8614513:0914514:11250601251291691Pockmark field. 3D-6714514:1114515:12251292251978687Pockmark field. 3D-8714515:1214516:08251979252605627Pockmark field. 3D-6814516:0814517:13252606253319714Pockmark field. 3D-8814517:1314518:13253320253989670Pockmark field. 3D-6914518:1314519:14253990254673684Pockmark field. 3D-8914519:1414520:26254674255475802Pockmark field. 3D-7114520:2614521:25255476256136661Pockmark field. 3D-9014521:2514522:38256137256942806Pockmark field. 3D-7014522:3814523:35256943257580638Pockmark field. 3D-9114523:351460:44257581258350770Pockmark field. 3D-721460:441461:41258351258989639Pockmark field. 3D-921461:411462:56258990259823834Pockmark field. 3D-731462:561464:08259824260628805Pockmark field. 3D-931464:081465:10260629261317689Pockmark field. 3D-741465:101466:21261318262111794Pockmark field. 3D-941466:211467:29262112262866755Pockmark field. 3D-751467:291468:30262867263542676Pockmark field. 3D-951468:301469:29263543264203661Pockmark field. 3D-761469:2914610:32264204264902699Pockmark field. 3D-9614610:3214611:25264903265485583Pockmark field. 3D-7714611:2514612:21265486266101616Pockmark field. 3D-9714612:2114613:22266102266784683Pockmark field. 3D-7814613:2214614:27266785267509725Pockmark field. 3D-9814614:2714615:27267510268177668Pockmark field. 3D-7914615:2714616:31268178268892715Pockmark field. 3D-9914616:3114617:37268893269624732Pockmark field. 3D-8014617:3714618:47269625270413789Pockmark field. H-1114618:4714619:50270414271112699Extra Huntec Line H-1214619:5014620:35271113271612500Extra Huntec Line3D-99a14620:3514621:10271613272006394Pockmark field.  Appendix 3. Reftek receiver station locations and elevations, reoccupations of 1998 SHIPS sites, and estimates of signal propagation. Maximum1998Range ofEastingNorthingFinalReftekReftekSHIPSFirst-ReceiverDASUTM 10,UTM 10,Elev.LatitudeLongitudeStation.Arrivals,No.No.metersmeters(m)NAD 83WGS 84No.kilometers101608849440554034172548.78373-123.0761620102611948046654092211748.83566-123.2661910103759147572754144864948.88285-123.331087104759546988754175528448.91018-123.4109711019181057333463293542221411148.95176-123.5013735106759945752154270834248.99519-123.58071110202010776024530105432388449.04258-123.643001610876204496715438036849.09312-123.6893830109760144883054425021549.13322-123.7014711021161107280441701544497112549.15479-123.7995414111761943861454488596149.18946-123.842471102220112601948278253982622648.73714-123.2341830113610747802654069113548.81480-123.2993230114760546846654033107248.78199-123.4292635115729646422954133372148.87196-123.4878120116734445677754204005248.93502-123.590172011774514508045424432648.97084-123.6722220118728844840354296852949.01790-123.7056825119609645260154076676648.82018-123.64572-120731944636254190535948.92209-123.7321912121731644234354322944349.04083-123.788932012274534385825439378----1237296428352544578324049.16068-123.9827435124704849353154275194649.00054-123.0884511030812570644878755438311249.09753-123.1661011031012676044853655450590349.20793-123.20093110320127708148094354652147949.33935-123.26233181287283460532547327213849.41085-123.54409201297065454848547573515849.43261-123.622731104318130709144342554799352849.46943-123.780861104428150710350580453945395248.70386-122.921125151728450969353947081548.70533-122.8682524152744351781853886414048.65057-122.75808261537317516468539074513148.66954-122.7763224154746253289153805362348.57705-122.5540810075155745853748353887444448.65063-122.49108100612156709853754153945522348.70287-122.4897713157611153847554059097148.80498-122.476020158743352607554032733048.78191-122.645057159761352726154006273648.75806-122.6290810160759652437253982001948.73634-122.668541016176115258315396160548.71793-122.6488210162733652141853986696848.74067-122.70869100411163742952298253956873148.71379-122.687581316474455249025393778548.69654-122.6615916165745752633253926146448.68601-122.64223100526166759451590754148212648.88614-122.7830113167744851365654209783248.94158-122.8135110 Appendix 4. Statistics of GPS Reftek station locations and elevations Time ofTime ofNo. ofNo. ofLocationElev.StationDASFirst LockLast TimeLocksLocksSt. Dev.St. Dev.No.No.Dy:Hr:MnDy:Hr:MnUsedRejected(m)(m)1016088134:21:06140:22:4689309.315.11026119135:15:09140:17:4751145.914.91037591134:19:01140:18:46110346.114.31047595134:21:08140:20:46107375.713.21057333134:21:45146:14:57208724.411.51067599134:22:34146:14:43215565.614.21077602134:17:56147:23:46250696.416.11087620134:17:07147:22:55239689.924.71097601134:22:38147:20:47228786.416.51107280134:23:42147:20:26243676.316.41117619134:21:44147:19:52239686.518.31126019134:00:43140:00:46107365.812.71136107134:15:36136:20:4649205.617.41147605134:01:50140:22:48123318.620.41157296134:00:23140:19:49124401167344133:23:39147:17:00249817.920.11177451133:21:21147:16:48259746.318.21187288133:20:32147:17:47262706.816.41196096130:23:34135:05:4639268.182.21207319133:18:51139:15:16112306.318.31217316133:18:03147:17:48253757.617.01227453133:17:00-----1237296141:23:33147:17:00104299.525.21247048134:02:49141:00:591381213.6634.21257064133:23:51146:16:46209644.612.11267604133:22:41143:15:4674274.910.91277081133:21:15146:22:491604510.920.01287283133:18:01146:22:46242767.519.71297065133:17:11146:21:45235766.314.61307091133:15:50146:21:46246736.815.71507103131:19:54139:16:59131396.816.71517284131:18:32139:16:46139477.116.31527443131:16:27139:17:421494511.730.01537317131:15:06139:17:48156366.615.11547462131:23:13140:02:00144526.614.31557458132:01:40138:23:55163113.11959.71567098132:03:27138:23:55116396.615.51576111132:02:26139:01:41129407.416.91587433133:19:38138:18:48418.853.31597613133:19:05139:21:46110385.213.71607596133:18:26139:19:46110379.927.01617611133:19:26139:20:46116325.914.61627336132:21:36139:19:49127405.013.01637429132:20:28139:18:47133335.213.21647445132:19:10139:18:48136338.015.81657457132:20:08139:17:53116385.316.31667594132:15:43139:14:46124445.413.41677448132:17:26139:15:48129396.819.3Median133396.616.4 Appendix 5: Receiver DAS numbers, quality of timing, tape numbers, and comments. Station No. DAS No. Quality of TimingDDS-3 3-comp. tapes (IRIS) Comments1016088good1/151026119errors1/30aFixed timing error, 139:23:47 to 140:03:421037591good1/171047595good2/51057333good2/51067599good1/171077602good1/171087620good1/171097601errors1/17Possible 1-sec error from 141:17:00 to 141:19:001107280good2/51117619good1/30a1126019errors1/30aShort data segments; GPS failed at 139:11:301136107good1/151147605errors1/30aFixed timing error, 138:09 to 138:10 (still 8-msec error?)1157296good2/101167344good2/51177451good1/30a1187288good2/101196096good1/151207319good2/51217316good2/51227453---1237296good2/101247048errors1/15GPS failed at 141:01:021257064good1/151267604errors1/30a136:18:46-139:18:00 missing; no GPS locks after 141:00:541277081good1/151287283good2/51297065good1/151307091good1/171507103good1/131517284good1/131527443good1/131537317good1/131547462good1/30a1557458good1/131567098good1/131576111good1/131587433errors1/30aFixed timing error, 133:19:43 to 135:18:381597613good1/131607596good1/131617611good1/131627336good1/131637429good1/131647445errors1/30aFixed 2 timing errors at 136:11:45 and 138:13:461657457good1/13Missing header - manually set sample rate, gains and format1667594good1/13Errors during ref2segy1677448good1/13 Appendix 6. PASSCAL SEGY Trace Header Format Byte # Description 1 - 4 Trace sequence number within data stream 5 - 8 Trace sequence number within reel (same as above) 9 - 12 Event number (FFID number) 13 - 16 Channel number = 1 or 4 for the vertical component, 2 or 5 for the N-S horizontal component, 3 or 6 for the E-W horizontal component 17 - 20 Energy Point number (FFID) | 29 - 30 Trace identification code = 1 for seismic data | 33 - 36 Source-receiver offset (m) 37 - 40 Receiver elevation (m) 41 - 44 Source Elevation (depth) (m) | 69 - 72 Source X coordinate (UTM Easting) 73 - 76 Source Y coordinate (UTM Northing) 77 - 80 Receiver X coordinate (UTM Easting) 81 - 84 Receiver Y coordinate (UTM Northing) | 89 - 90 Coordinate units = 2 for Lat/Long | 103 - 104 Low 2 bytes of the total shift in milliseconds | 115 - 116 Number of samples in this trace (note if equal 32767 see bytes 229 - 232) 117 - 118 Sample interval in microsecs for this trace (note if equal 1 see bytes 201 - 204) 119 - 120 Fixed gain flag = 1 121 - 122 Gain of amplifier | 157 - 158 Year data recorded 159 - 160 Day of year 161 - 162 Hour of day (24 hour clock) 163 - 164 Minute of hour 165 - 166 Second of minute 167 - 168 Time basis code: 1=local 2=GMT 3=other | 174 - 174 Stake number index | 181 - 186* Station Name code (5 chars + 1 for termination) 187 - 194* Sensor Serial code (7 chars + 1 for termination) 195 - 198* Channel Name code (3 chars +1 for termination) 199 - 200* Extra bytes (2 chars) 201 - 204* Sample interval in microsecs as a 32 bit integer 205 - 206* Data format flag: 0=16 bit integer 1=32 bit integer 207 - 208* Milliseconds of second for first sample 209 - 210* Trigger time year 211 - 212* Trigger time Julian day 213 - 214* Trigger time hour 215 - 216* Trigger time minutes 217 - 218* Trigger time seconds 219 - 220* Trigger time milliseconds 221 - 224* Scale factor (IEEE 32 bit float) (true amplitude = (data value)*(scale factor)/gain 225 - 226* Instrument Serial Number 229 - 232* Number of Samples as a 32 bit integer 233 - 236* Max value in counts. 237 - 240* Min value in counts. *Header values not specified in the standard SEGY format Appendix 7. Minimum source-receiver offset (in meters) for each station for every Julian Day JD101102103104105106107108109110111112113114115116135109974172464210829186042591932492382504140548687534181249675091639016194242401363171943878641267419606264643265438256411564864153117674912369206511899725829137269752874904371722956615135282007224313303993536315146781328542131382516012520564435082443106120835348958913031178742333217189873034361394637534875279132229015334983272285893471398741281145462349272414816556140526374005233212282182234717849129538066393486881177041766312722454214125387216281750112017790110996128602824014220408154181201810883107491803621868221391432561821778189871728215899220902482828402144254742144018339164131493421211240582810914524869215961939518272171812367926645280991462343620092180291721616508232972652526600JD1171181191201211221231241251261271281291301501511353108535247342684184329091360526121413845719462435728523674930136322893593636174425125764127482500740010543235932869370438182641371052214983146982150657471186337128497305448761098912670841382985176943134418153561661228342325533626444735394814225713914711125422165115186275001746612338144398962100711723660025622151402117416508160062192336246267582301418604899311001165961412546620463198952346735173249661768515615120871638522219142200171699320043313922487615310182742311633650143269092393626586352272072114688176482243132925144263492321725722344002427215109181782304433600145271152449827541369252288114398201792481335038146256872317226413366272167413273190322336633283JD152153154155156157158159160161162163164165166167135388529552764785995491661240694444813116116921562898795860113798136367735126887892511696212609460910853805465313028493086333457447470137326734431504115625157852133190598969526055292858285535054419494390521385238250008692496865666095627565203854227526425487749803526145523557059386143533013972055695788820686022824867709368081706196990172338673697053373239750795315048086Yellow boxes denote closest approaches less than 10 km. Red lettering denotes ranges between 10 and 20 km. Gray lettering denotes ranges between 30 and 40 km. Appendix 8. Local and regional earthquakes archived. FFID No. Year:JD:Hr:Mn:Sec Latitude LongitudeMag-nitudeDepth, km Source3000012002:131:19:10:01.0947.7962-122.77282.323.0UW3000022002:131:19:56:49.4646.7040-122.76773.26.4UW3000032002:131:21:22:00.5446.8270-117.18172.70.1UW3000042002:132:06:10:36.0048.9200-123.05000.422.0PGC3000052002:132:14:28:29.7248.5392-121.59930.55.9UW3000062002:132:18:39:31.7646.7145-122.76383.06.8UW3000072002:132:20:54:16.4446.4798-121.34132.12.2UW3000082002:133:04:22:15.0049.1800-128.94003.210.0PGC3000092002:133:13:47:32.0049.1500-122.66000.918.0PGC3000102002:133:21:00:37.0048.4000-123.51002.744.2PGC3000112002:133:21:21:47.1946.7065-122.77033.546.0UW3000122002:133:21:58:33.7348.0845-121.92432.00.0UW3000132002:133:23:29:14.4347.9192-122.71031.327.8UW3000142002:134:15:26:46.4848.7395-121.76771.320.9UW3000152002:134:17:05:30.2146.9098-122.30051.26.2UW3000162002:134:17:13:10.5547.8505-123.06022.147.7UW3000172002:134:21:33:16.7646.7085-122.77002.38.8UW3000182002:134:21:53:74.8244.2462-120.89622.70.0UW3000192002:134:22:50:19.2347.0095-122.00571.815.3UW3000202002:135:00:29:10.1947.7810-122.82831.024.2UW3000212002:135:01:28:42.6548.2935-122.20821.011.9UW3000222002:135:05:48:21.2748.6750-122.03580.95.3UW3000232002:135:06:26:53.9447.6607-121.81970.512.7UW3000242002:135:08:48:51.0947.8182-121.94620.127.6UW3000252002:135:11:15:14.0049.5500-127.10001.029.0PGC3000262002:135:17:54:48.6042.2313-121.90124.342.0UW3000272002:135:19:00:37.7247.7977-121.98650.20.0UW3000282002:135:21:11:57.7247.4587-120.65230.98.3UW3000292002:135:21:31:32.6046.7000-122.75322.710.0UW3000302002:136:04:19:33.6046.9978-122.00551.214.1UW3000312002:136:05:36:05.0048.9300-123.05000.324.0PGC3000322002:136:05:36:27.8547.6323-122.56770.922.4UW3000332002:136:05:52:27.0049.3900-128.72002.810.0PGC3000342002:136:05:59:55.8942.2318-121.90672.09.5UW3000352002:136:06:54:54.3547.6860-123.67750.838.5UW3000362002:136:20:31:54.4846.6928-122.79282.316.4UW3000372002:137:05:41:52.3442.2223-121.90422.13.8UW3000382002:137:06:39:34.5847.7075-123.66400.229.8UW3000392002:137:07:46:19.8247.0080-122.00081.415.7UW3000402002:137:21:12:13.1746.7115-122.77632.34.4UW3000412002:138:06:31:19.0048.7900-123.36000.418.0PGC3000422002:138:09:09:14.0048.9200-123.05000.623.0PGC3000432002:138:12:06:34.0049.3300-123.72001.02.0PGC3000442002:139:06:02:35.0049.1800-127.78001.610.0PGC3000452002:139:07:47:30.0847.7313-122.62420.226.3UW3000462002:139:10:50:43.0049.6800-127.08003.920.0PGC3000472002:139:17:05:27.6548.3000-122.19482.713.7UW3000482002:140:08:33:38.4147.6792-121.87750.112.1UW3000492002:140:10:44:38.9647.7783-122.86372.020.2UW3000502002:140:12:07:35.3147.7708-122.84931.420.5UW3000512002:141:00:13:56.2047.8323-122.04280.917.3UW3000522002:141:00:30:21.0147.6525-120.19180.90.5UW3000532002:141:10:40:47.0049.9200-127.84001.030.0PGC3000542002:141:19:06:40.4648.0923-121.91271.548.0UW3000552002:141:19:31:74.0848.4665-122.17730.50.0UW3000562002:141:21:03:20.8346.7063-122.77382.47.0UW3000572002:141:22:25:43.0048.7200-128.63002.710.0PGC3000582002:142:00:29:43.1047.8135-123.05881.524.8UW3000592002:142:03:41:52.0048.6400-124.74001.334.0PGC 3000602002:142:05:58:39.0147.0435-121.92000.419.9UW3000612002:142:18:44:26.1446.6220-120.54382.18.0UW3000622002:142:19:59:02.0049.1500-127.74001.710.0PGC3000632002:142:20:55:15.3146.7070-122.76233.210.7UW3000642002:143:01:19:09.1149.0073-122.53281.811.0UW3000652002:143:10:49:16.5848.4393-123.08281.117.1UW3000662002:143:18:04:35.3447.7775-122.84450.720.5UW3000672002:143:21:02:10.1446.7010-122.76283.08.8UW3000682002:143:21:43:49.8645.5573-123.36452.10.0UW3000692002:143:22:34:58.4146.9803-122.20221.31.5UW3000702002:143:23:05:37.6747.7708-122.84381.119.4UW3000712002:144:11:17:29.0648.0527-122.61751.029.5UW3000722002:144:13:57:17.0049.6900-127.07001.022.0PGC3000732002:144:14:09:29.0049.3600-123.94001.364.0PGC 3000742002:144:20:32:37.4646.5898-123.02282.54.0UW3000752002:144:21:07:56.7346.7002-122.76783.37.0UW3000762002:144:22:40:76.3145.3330-121.68282.03.2UW3000772002:146:02:17:32.0048.8700-123.45000.220.0PGC3000782002:146:10:21:53.8247.7048-120.11282.02.4UW3000792002:146:14:04:21.4348.1825-120.17031.80.6UW3000802002:147:08:43:58.6148.2040-120.17172.41.3UW3000812002:147:11:41:37.1947.7842-122.82230.923.4UW3000822002:147:17:41:21.0048.6300-128.88002.610.0PGC3000832002:147:17:52:33.3846.7082-122.75682.98.2UW3000842002:147:19:33:38.7746.9372-121.96822.413.2UW3000852002:147:21:47:39.0048.7600-128.57002.310.0PGC3000862002:147:22:56:56.0048.8100-128.52002.610.0PGCSources: Pacific Geoscience Centre (PGC), University of Washington (UW). Appendix 9. Teleseisms archived to tape. FFIDYRJDHr:MnSecLatitudeLongitudeMag.Depth400001200213223:1252.91-1.1430127.08705.533.0400002200213319:5443.1219.1410121.23805.533.0400003200213319:5722.9019.1320121.23805.533.0400004200213414:1903.383.5070125.37705.533.0400005200213416:5610.42-36.518078.93205.610.0400006200213503:2735.58-21.4050-174.26105.710.0400007200213503:4605.7624.6360121.92205.710.0400008200213710:4010.7748.1680-27.80805.710.0400009200213815:1508.80-2.907033.73305.810.0400010200214106:0259.9417.7790-81.91105.910.0400011200214120:0416.1644.4300146.61905.9149.8400012200214315:5215.28-30.7490-71.19705.952.1400013200214322:0551.82-5.8160102.06406.010.0400014200214400:2315.93-31.9710-70.94706.260.2400015200214505:3631.9753.8150-161.11606.333.0400016200214600:1021.041.8320127.23806.5109.0Source: National Earthquake Information Center (NEIC) PAGE  PAGE 25 !9qrno  "9Zgst  56;!!"""0"""$#(#)#.#m%q%r%x%%%N&U&''''((((****++++:, >*OJQJ5>*OJQJ5 5OJQJCJEH OJQJOJQJW 789a  !9:;<=>?@AB@d $@d $@d 789a  !9!!""0"1"$2(*d[ppqr~st7uvw xxyrzo{H|}}}}}~9:::::":$:&:(:):>BCDEFGHIJnopqn$@d$@d@d"#9Sq9Z|.Jg $$d$$d$d$~d$@d$+dghst/y-s!M~d$d$d d $dd$~d$$dMs  !!""0"1"$2(*S-.~hd~d$~d$~d~d$@d@d$d:,>,?,D,k,o,p,u,.0.b.f.g.l.....447788<<;?P?R?j???}@@yAABBCDG GeGkGGGHH1J:JKK.M1MmMoMEQ^QSS^^a abvcde*fgggggg"h5hhhi!i 6OJQJ B*OJQJ5B*OJQJB*OJQJnH  CJOJQJ >*OJQJOJQJ 5OJQJP../.0.2444[67888E9A:;<<<:?;?Q?R?j?CC$d$$~d~hd~dCCDEGHHHHHIIJJ>K?KKKKKKnMOCQDQEQ ~d~d$d$dEQ]Q^QRSSSSSVVY\^^^^^ aaa aavcd+fd$d$$d~d~d$~d+fgg!h"h4h5hh7iKjklmdno$hd !$$hd "$$d $$hdh$hd $$hd !$$dpd$d!i7ij;jKjjjjkkkEnLnooo,pJppqrrrrrYs`s}sttt u%vSvwwxxxxy3zAzCzI{^{o{{{ |G||}}}}}~~"no{5B*CJOJQJnH B*CJOJQJnH 5CJOJQJ6CJOJQJ CJOJQJ 6OJQJ6B*OJQJnH B*OJQJnH 6OJQJEoo[ppqr~st7uvw xx$$hd " $$hd$hd " $hd $hd$$hd "$$d $d "hd xyrzo{H|}}}}}~~~ ~~~~~$d8$$d8$@d @0d@hd $$hd "hd $$hd$$hd ~~~~~"~,~.~:~B~D~M~T~^~e~$d8$$d8$e~f~m~r~v~x~{~~~~~~~zrrrrrrrrrrr$d8$$$ g >.^ ~~~~~~~~~~~~~~~~~~~ &'.$d8$$$ g >.^.37:<BIQT\fgnswz|$$ g >.^$d8$ &'.37:<$$ g >.^$d8$<BIQT\fgnswz|€ɀ$$ g >.^$d8$ɀрԀ܀ &'.37:<BIQT$$ g >.^$d8$T\fgnswz|ÁʁҁՁ݁$$ g >.^$d8$ '(/48:<BIQT\fgn$d8$$$ g >.^nswy{‚ɂтԂ܂$$ g >.^$d8$ '(/48:<BIQT\fgnswy{$$ g >.^$d8${ȃЃӃۃ$$ g >.^$d8$%&-269;AHPS[efmrvy{$$ g >.^$d8$ȄЄӄۄ%$$ g >.^$d8$%&-269;AHPS[efmrvy{$d8$$$ g >.^ȅЅӅۅ%&-26$$ g >.^$d8$69;AHPS[efmrvy{$$ g >.^$d8$ȆІӆۆ%&-268:@G$$ g >.^$d8$GORZdelquwyŇ͇Ї$$ g >.^$d8$Ї؇ !").246<CKNV`$$ g >.^$d8$`ahmqsu{Ɉ̈Ԉވ߈$d8$$$ g >.^ %*.028?GJR\]dim$$ g >.^$d8$moqw~Ɖɉщۉ܉$$ g >.^$d8$ #(,/17>FIQ[\chloqw~$$ g >.^$d8$~ƊɊъۊ܊ $$ g >.^$d8$ #(,/29@HKS]^ejnqt{$$ g >.^$d8$‹ʋ͋Ջߋ  '$d8$$$ g >.^',035;BJMU_`glpsu{$$ g >.^$d8$Œʌ͌Ռߌ  ',035$$ g >.^$d8$5;BJMU_`glprtz$$ g >.^$d8$ȍˍӍݍލ $)-/17>FI$$ g >.^$d8$IQ[\chlnqxȎˎӎݎ$$ g >.^$d8$ݎގ $)-/17>FIQ[\c$d8$$$ g >.^chlnqw~ȏˏӏݏޏ$$ g >.^$d8$ %*.139@HKS]^ejnqs$$ g >.^$d8$syȐːӐݐސ$$ g >.^$d8$ %*.139@HKS]^ejnqsy$$ g >.^$d8$ȑˑӑݑޑ $$ g >.^$d8$%*.139@HKS]^ejnqsy$d8$$$ g >.^ǒʒҒܒݒ #(,$$ g >.^$d8$,.06=EHPZ[bgkmou|$$ g >.^$d8$ÓƓΓؓٓ $(*,29$$ g >.^$d8$9ADLVW^cgikqx”$$ g >.^$d8$”ʔԔՔܔ  $')/6>AIS$$ g >.^$d8$ST[`dgiov~ɕӕԕە$d8$$$ g >.^ە  $')/6>AIST[`d$$ g >.^$d8$dgiov~ɖӖԖۖ$$ g >.^$d8$  $')/6>AIST[`dgiov$$ g >.^$d8$v~×˗՗֗ݗ$$ g >.^$d8$ "&(*07?BJTU\aegiov~$$ g >.^$d8$ȘҘӘژߘ$d8$$$ g >.^"$&,3;>FPQX]acekrz}$$ g >.^$d8$ęΙϙ֙ۙߙ !#$$ g >.^$d8$#)08;CMNUZ^acipx{$$ g >.^$d8$Ú͚Κ՚ښޚ !#)08;$$ g >.^$d8$;CMNUZ^acipx{śϛ$$ g >.^$d8$ϛЛכܛ!$&,3;>FPQX$d8$$$ g >.^X]acekrz}ĜΜϜ֜ۜߜ$$ g >.^$d8$ߜ  "(/7:BLMTY]_a$$ g >.^$d8$agnvyʝ˝ҝם۝ݝߝ$$ g >.^$d8$ $+36>HIPUY[]cjru$$ g >.^$d8$u}ƞǞΞӞמڞܞ$$ g >.^$d8$")14<FGNSWZ\biqt|$d8$$$ g >.^ƟǟΟӟןڟܟ$$ g >.^$d8$")14<FGNSWZ\biqt|$$ g >.^$d8$ƠǠΠӠנڠܠ#*$$ g >.^$d8$*25=GHOTX[^eltw$$ g >.^$d8$ɡʡѡ֡ڡݡ  &-58@J$$ g >.^$d8$JKRW[]_eltwȢɢТ$d8$$$ g >.^Тբ٢ۢݢ")14<FGNSW$$ g >.^$d8$WY[ahps{ģţ̣ѣգף٣$$ g >.^$d8$٣ߣ %-08BCJOSUW]d$$ g >.^$d8$dlow¤ɤΤҤդפݤ$$ g >.^$d8$ $,/7ABINRUW]dlow$$ g >.^$d8$¥ɥΥҥեץݥ $d8$$$ g >.^ $,/7ABINRUW]dlow$$ g >.^$d8$¦ɦΦҦզצݦ $$ g >.^$d8$$,/7ABINRUW]dlow$$ g >.^$d8$§ɧΧҧէקݧ #+.$$ g >.^$d8$.6@AHMQSU[bjmu$$ g >.^$d8$ƨ˨ϨѨӨ٨ '*2<=D$d8$$$ g >.^DIMOQW^fiq{|©ǩ˩$$ g >.^$d8$˩ͩϩթܩ #&.89@EIKM$$ g >.^$d8$MSZbemwxĪȪ˪ͪӪڪ$$ g >.^$d8$ڪ "%-78?DHKMSZbe$$ g >.^$d8$emwxīȫ˫ͫӫګ$$ g >.^$d8$ "%-78?DHKMSZbemwx$d8$$$ g >.^ĬȬˬͬӬڬ$$ g >.^$d8$ "%-78?DHKMSZbemwx$$ g >.^$d8$ĭȭ˭ͭӭڭ $$ g >.^$d8$!$,67>CGIKQX`ckuv}$$ g >.^$d8$ŮǮɮϮ֮ޮ (2$$ g >.^$d8$23:?CEGMT\_gqry~$d8$$$ g >.^ïů˯үگݯ $./6;?$$ g >.^$d8$?ACIPX[cmnuz~ð$$ g >.^$d8$ðɰаذ۰ #-.5:>ACIP$$ g >.^$d8$PX[cmnuz~ñɱбر۱$$ g >.^$d8$۱ #-.5:>ACIPX[cm$$ g >.^$d8$mnuz~òɲвز۲$d8$$$ g >.^ #-.5:>ACIPX[cmnuz~$$ g >.^$d8$~³ij˳ҳڳݳ$$ g >.^$d8$ $./6;?ACIPX[cmnuz~$$ g >.^$d8$Ǵδִٴ $$ g >.^$d8$ *+27;=?ELTW_ijqvz|~$$ g >.^$d8$õʵҵյݵ &'.$d8$$$ g >.^.37:<BIQT\fgnswz|$$ g >.^$d8$¶ɶѶԶܶ &'.37:<$$ g >.^$d8$<BIQT\fgnswz|·ɷ$$ g >.^$d8$ɷѷԷܷ &'.37:<BIQT$$ g >.^$d8$T\fgnswz|¸ɸѸԸܸ$$ g >.^$d8$ &'.37:<BIQT\fgn$d8$$$ g >.^nswy{ǹϹҹڹ$$ g >.^$d8$#$+0468>EMPXbcjosuw$$ g >.^$d8$w}ú˺κֺ$$ g >.^$d8$  ',024:AILT^_fkoqsy$$ g >.^$d8$ǻʻһܻݻ $$ g >.^$d8$$)-028?GJR\]dimprx$d8$$$ g >.^ǼʼҼܼݼ $)-$$ g >.^$d8$-028?GJR\]dimprx$$ g >.^$d8$ǽʽҽܽݽ $)-028?$$ g >.^$d8$?GJR\]dimprxǾʾ$$ g >.^$d8$ʾҾܾݾ $$ g >.^$d8$ !ou{zssskkhkhkk$$d8$@d$$ g >.^ ƿϿ{{{{{{ud8$$d8$o$$ _a c #g$d8$$$ ϿпRS`a*+no78{|HIXY!"de01gh CDz{UVB*CJOJQJnH 5B*OJQJnH 5B*CJOJQJnH B*OJQJnH UϿпҿֿۿ߿ze$$ _a c #gd8$$d8$$d8$o$$ _a c #g  &-48RSUY_cipw|$$ _a c #gd8$$d8$$d8$ $*.4;BF  $$ _a c #gd8$$d8$$d8$F`acgmqw~  $d8$$d8$$$ _a c #gd8$ *+.28<AHOTnorv{ $$ _a c #gd8$$d8$$d8$ 78$d8$$$ _a c #gd8$$d8$8;?EIOV]a{|$$ _a c #gd8$$d8$$d8$ ").HILPVZ`gnr$$ _a c #gd8$$d8$$d8$r$d8$$d8$$$ _a c #gd8$"&,3:>XY\`fjov}$$ _a c #gd8$$d8$$d8$!"&*/38?FJde   $d8$$$ _a c #gd8$$d8$eimrv{$$ _a c #gd8$$d8$$d8$ 0148>BHOVZghkouy$$ _a c #gd8$$d8$$d8$ $d8$$d8$$$ _a c #gd8$$+26CDGKQU[bimz{~$$ _a c #gd8$$d8$$d8$ $d8$$$ _a c #gd8$$d8$"&+/4;BFUVY]cgmoqsԴԴ$$ _a c #gd8$$d8$$d8$ $$ _a c #gd8$$d8$$d8$ #'-17>EIXY\`fjpw~$d8$$d8$$$ _a c #gd8$ XY<=uv"#[\ ';<QXst@A PQab,-no67z{DEDEB*CJOJQJnH B*OJQJnH B*CJOJQJnH Z "$$ _a c #gd8$$d8$$d8$")-<=@DJNT[bfuvy}$d8$$$ _a c #gd8$$d8$"#&*04$$ _a c #gd8$$d8$$d8$4:AHL[\_cimry$$ _a c #gd8$$d8$$d8$  ',;<?C$d8$$d8$$$ _a c #gd8$CHLQX_dstw{$$ _a c #gd8$$d8$$d8$ "&@ADHNRX_fk$d8$$$ _a c #gd8$$d8$   $$ _a c #gd8$$d8$$d8$#*16PQTX]afmty $$ _a c #gd8$$d8$$d8$ $*.4;BGabfj$d8$$d8$$$ _a c #gd8$jptz$$ _a c #gd8$$d8$$d8$,-049=BIPTnorv{ $d8$$$ _a c #gd8$$d8$ 67:>CG $$ _a c #gd8$$d8$$d8$GMT[`z{~$$ _a c #gd8$$d8$$d8$ &-1DEKOUY_fmq$d8$$d8$$$ _a c #gd8$ &$$ _a c #gd8$$d8$$d8$&-1DEKOUY_fmq$d8$$$ _a c #gd8$$d8$89vw01no-.mn-.mn./op*+hi#$ab]^]^^_]^B*OJQJnH B*CJOJQJnH ^ !%89?CHL$$ _a c #gd8$$d8$$d8$LQX_cvw}$$ _a c #gd8$$d8$$d8$ 017;@DIPW[nouy$d8$$d8$$$ _a c #gd8$y~$$ _a c #gd8$$d8$$d8$-.48>BHOVZmntx~$d8$$$ _a c #gd8$$d8$-.48>B$$ _a c #gd8$$d8$$d8$BHOVZmntx~$$ _a c #gd8$$d8$$d8$./59?CIPW\opvz$d8$$d8$$$ _a c #gd8$z $$ _a c #gd8$$d8$$d8$ *+15:>CJQUhiosx|$d8$$$ _a c #gd8$$d8$ #$*.37$$ _a c #gd8$$d8$$d8$7<CJNabfjosx$$ _a c #gd8$$d8$$d8$ $(.28?FJ]^dh$d8$$d8$$$ _a c #gd8$hnrx$$ _a c #gd8$$d8$$d8$ %)/39@GJ]^eiosy$d8$$$ _a c #gd8$$d8$ %)/3$$ _a c #gd8$$d8$$d8$39@GK^_eiosy$$ _a c #gd8$$d8$$d8$ %)/38?FJ]^dh$d8$$d8$$$ _a c #gd8$hmqv}$$ _a c #gd8$$d8$$d8$"'+07>BUV\`einu|$d8$$$ _a c #gd8$$d8$UVMNBCDEGH/0mn'(ef ]^^_^_^_YZB*OJQJnH B*CJOJQJnH ^#$$ _a c #gd8$$d8$$d8$#(/6:MNUY^bhovz$$ _a c #gd8$$d8$$d8$ $+/BCIM$d8$$d8$$$ _a c #gd8$MSW]dko$$ _a c #gd8$$d8$$d8$ &-1DEKOUY_fmq$d8$$$ _a c #gd8$$d8$$$ _a c #gd8$$d8$$d8$")04GHOSY]cjqu$$ _a c #gd8$$d8$$d8$ /06:$d8$$d8$$$ _a c #gd8$:?CHOVZmntx}$$ _a c #gd8$$d8$$d8$ '(.27;@GNRef$d8$$$ _a c #gd8$$d8$flpuy~$$ _a c #gd8$$d8$$d8$  &*/38?FJ]^dhnrx$$ _a c #gd8$$d8$$d8$ %)$d8$$d8$$$ _a c #gd8$)/39@GK^_eiosy$$ _a c #gd8$$d8$$d8$ %)/39@GK^_$d8$$$ _a c #gd8$$d8$_eiosy$$ _a c #gd8$$d8$$d8$ %)/39@GK^_eiosy$$ _a c #gd8$$d8$$d8$"&$d8$$d8$$$ _a c #gd8$&+/4;BFYZ`dimry$$ _a c #gd8$$d8$$d8$#',3:>QR$d8$$$ _a c #gd8$$d8$QR LM LM KLSTVXdegiz{} 12ef:;stGHB*CJOJQJnH 5B*CJOJQJnH 5B*CJOJQJnH OJQJB*OJQJnH B*CJOJQJnH NRX\aejqx|$$ _a c #gd8$$d8$$d8$ !'.59LMSW]agnuy$$ _a c #gd8$$d8$$d8$y $d8$$d8$$$ _a c #gd8$!'.59LMSW]agnuy$$ _a c #gd8$$d8$$d8$  &-48KL$d8$$$ _a c #gd8$$d8$LQU[_elsw$$ _a c #gd8$$d8$$d8$TUVWXYZ[\d~~$$d8$@do$$ _a c #g defghijklqz{|Xp$$ B < $$d8$o$$ B <  |} ($d8$$$$$ B < $$d8$"&126;BJMVabe$d8$o$$ B < $d8$efjov~$d8$$d8$$$ B <  "+67:;?DKSV_jps$d8$$$ B < $d8$stx}$d8$$d8$$$ B <  #+/8CDGHLQX`clw}$d8$$$ B < $d8$$d8$$d8$$$ B < PQRSLM&'_`/0fg89lm ?@rs]^`h5B*CJOJQJnH OJQJB*CJOJQJnH B*CJOJQJnH Q !&-58ALMPQUZailu$d8$$$ B < $d8$$d8$$d8$$$ B < #(/7:CNORSW\cknw$d8$$$ B < $d8$$d8$$d8$$$ B <  &.09DJLMQV]egp{$d8$$$ B < $d8$$d8$$d8$$$ B <  #&'+07?BKV\_`dipx{$d8$$$ B < $d8$ $d8$$d8$$$ B <  +,/049@HKT_dfgkpw$d8$$$ B < $d8$ $d8$$d8$$$ B < !*5689=BIQT]hilmqv}$d8$$$ B < $d8$ $$d8$$d8$$$ B < $'0;<?@DIPXZcnorsw|$d8$$$ B < $d8$$d8$$d8$$$ B < ^_`hpw~~$$d8$@do$$ B <  $$, 3g$d8$d$$ִ, 3g,-YZ?@mn%&/9RS12;E^_67denxJKxyB*CJOJQJnH B*OJQJnH B*CJOJQJnH B*CJOJQJnH 5B*CJOJQJnH 5B*CJOJQJnH L  #',-$$, 3gd$$ִ, 3g$d8$-16@JMPTYZ^cmw{~$$, 3g$d8$ %/36:$d8$$$, 3g:?@DIS]adhmnrw$$, 3g$d8$  %&*/9CF$$, 3g$d8$FIMRSW\fptw{$$, 3g$d8$ !%(,126;E$$, 3g$d8$EORTY^_chr|x$$, 3g$d8$ $(+067;$$, 3g$d8$;@JTX[_deinx$$, 3g$d8$ !&0:>AEJ$$, 3g$d8$JKOT^hlosxy}$d8$$$, 3g !%(,126;EOSU$$, 3g$d8$12abDErs*+XYGH\]fm$+abuv78LM`avw5CJOJQJCJ CJOJQJOJQJB*CJOJQJnH B*CJOJQJnH TUZabfku$$, 3g$d8$   *48;?DEINXb$$, 3g$d8$bfimrsw|$$, 3g$d8$!%*+/4>HLOSXY]b$$, 3g$d8$blvz}l$d8$$$, 3g$d8$  r$d8H$5$7$8$9D$$d8$$d8$d8$$d$$ִ, 3g  &;<=>GHLQV[\T$d8$A$$r~L nbd8$$d8$ \]afmsgTA$$r~L &&n&&bd8$$d8$$d8$A$$r~L &&n&&b PPT$d8$$d8$A$$r~L &&n&&bd8$ $+0abTTPd8$$d8$$d8$A$$r~L &&n&&bbfkptuvzXTA$$r~L &&n&&bd8$$d8$$d8$78<AFKLMQVHTPA$$r~L &&n&&bd8$$d8$$d8$V[_`aejouvw{XTT$d8$A$$r~L &&n&&bd8$$d8$PP@d8H$5$7$8$9D$$d8$$d8$A$$r~L &&n&&bd8$01:A  ( ) > ? S T h i } ~             ( ) 2 9 p q        1 : L W \9B*CJOJQJnH CJ CJOJQJ>*CJOJQJ 5OJQJ5CJOJQJCJOJQJ CJOJQJM %*TT$d8$A$$r~L &&n&&bd8$$d8$*/015:AGDTP$d8$$d8$A$$r~L &&n&&bd8$TTT$d8$$d8$A$$r~L &&n&&bd8$        " ' ( ) TTTXd8$$d8$$d8$A$$r~L &&n&&b) - 2 7 = > ? C H M R S T X ] b g h i m TTTA$$r~L &&n&&bd8$$d8$$d8$m r w | } ~               TTA$$r~L &&n&&bd8$$d8$$d8$                   " TTT$d8$A$$r~L &&n&&bd8$$d8$" ' ( ) - 2 9 ? p q u z          @$d8$$d8$A$$r~L &&n&&bd8$           Tg``@dA$$r~L &&n&&b$d8$$d8$A$$r~L &&n&&bd8$  1 X   $    ? I q    Bs<F~@d8$d%d&d'd@d8$d%d&d'd~] ?f U^Fp@d8$d%d&d'd5/\  !%$d$$$d$$@d@d8$d%d&d'd%)-159$d$$9:>DI80(($d$$$d$$$$zJZj z"2"$B')9:>DNZ`l~+7=BCRSW]c'3BHPV\]eqλλױױλB*CJOJQJnH B*CJOJQJnH CJOJQJnH B*CJOJQJnH CJOJQJnH B*CJOJQJnH B*CJOJQJnH B*CJOJQJnH B*CJOJQJnH BINTZ`flrx~$d$$6$$:JZj z"2"$B') $d$$ %+X$d$$6$$:JZj z"2"$B') $d$$+17=BCHMRSW]chmrw|\$d$$9$$:JZj z"2"$B') "$d$$l$d$$9$$:JZj z"2"$B') "$d$$ !'-38=BHIJPV\`$d$$3$$:JZj z"2"$B') $d$$\]abcdekqw}$d$$$d$$3$$:JZj z"2"$B') q} '9EIOPXdv $017?DJPhqrvػB*CJOJQJnH B*CJOJQJnH B*CJOJQJnH CJOJQJnH CJOJQJnH B*CJOJQJnH B*CJOJQJnH B*CJOJQJnH F$d$$$d$$2$$:JZj z"2"$B')     $d$$$d$$'$$:JZj z"2"$B')!'-39?EFGHIOPTUVWX^djp$d$$'$$:JZj z"2"$B')$d$$pv|$d$$'$$:JZj z"2"$B')$d$$0H$$zJZj z"2"$B')$d$$$$&JZj z"2"$B')$d$$$d$$ $d$$  $*08H0(($d$$$d$$$$zJZj z"2"$B')017=>?DJPV\bhmqrv|L$d$$9$$:JZj z"2"$B') "$d$$8$d$$9$$:JZj z"2"$B') "$d$$ !"',-.4:;A4$d$$9$$:JZj z"2"$B') "$d$$!",.;AMSY_`dpqw} %+CIKLP\^deklrغغغغغB*CJOJQJnH B*CJOJQJnH B*CJOJQJnH B*CJOJQJnH B*CJOJQJnH CJOJQJnH B*CJOJQJnH IAGMSY_`djpqw}~T$d$$.$$:JZj z"2"$B') $d$$,$d$$6$$:JZj z"2"$B') $d$$ %+17=CIJK0$d$$$d$$5$$:JZj z"2"$B') KLPV\]^deklrsy$d$$$d$$'$$:JZj z"2"$B')$d$$'$$:JZj z"2"$B')$d$$ "$*+1289EKQSTXdflmstz{ 9?@DXdغİB*CJOJQJnH B*CJOJQJnH B*CJOJQJnH B*CJOJQJnH B*CJOJQJnH CJOJQJnH B*CJOJQJnH B*CJOJQJnH E "#$*+1289?EK$d$$'$$:JZj z"2"$B')$d$$KQRSTX^deflmstz{$d$$'$$:JZj z"2"$B')$d$$8H0(($d$$$d$$$$zJZj z"2"$B')$d$$$$&JZj z"2"$B')$d$$$d$$8P0(($d$$$d$$$$zJZj z"2"$B') "',049?@DINSX^\$d$$8$$:JZj z"2"$B') $d$$^dinsx}d$d$$9$$:JZj z"2"$B') "$d$$      $ * 0 6 $d$$9$$:JZj z"2"$B') "$d$$H T U   X!Y!\!]!!!!!""""L"P"T"W""""""""""###6#:#>#A#p#t#x#{#########"$&$+$/$^$b$g$j$$$üCJOJQJnH >*CJOJQJ CJOJQJOJQJCJ CJOJQJB*CJOJQJnH B*CJOJQJnH B*CJOJQJnH B*CJOJQJnH B*CJOJQJnH B*CJOJQJnH =6 < B H N T U Y _ e k q w }           Д$d$$'$$:JZj z"2"$B')$d$$   %!Y!Z!81111@d$$zJZj z"2"$B')Z![!\!]!!!!!!!!!!!!!!$d$$d$$$d$$d$@d!!!!""""""%":"B"L"u$$l !$d$$$d$$$d$$$d$$W$$l֞ ! L"P"T"W"X"_"t"|"""""""""""""""""$d$$$$l !$d$$$d$$$d$$""#####$#,#6#:#>#A#B#I#^#f#p#t#x#{#|###$$l !$d$$$d$$$d$$$d$$################$$"$&$+$/$0$7$$$l !$d$$$d$$$d$$$d$$7$L$T$^$b$g$j$k$r$$$$$$$$$$$$$$$$$$l !$d$$$d$$$d$$$d$$$$$$$$$%%%%I%M%Q%T%%%%%%%%%%%&&2&6&;&>&m&q&v&y&&&&&&&&&'!'&')'X'\'a'd''''''''' ((((D(H(L(O(~((((((((((()0)4)9)<)k)o)t)x)))))))))*CJOJQJnH  CJOJQJ_$$$%%%%%%"%7%?%I%M%Q%T%U%\%q%y%%%%%$$l !$d$$$d$$$d$$$d$$%%%%%%%%%%%%%%%&&& & &(&2&6&;&$d$$$d$$$d$$$d$$$$l !;&>&?&F&[&c&m&q&v&y&z&&&&&&&&&&&&&&$d$$$d$$$d$$$$l !$d$$&&&&& '''!'&')'*'1'F'N'X'\'a'd'e'l''''$d$$$d$$$$l !$d$$$d$$'''''''''''''''( ((((((2(:($d$$$$l !$d$$$d$$$d$$:(D(H(L(O(P(W(l(t(~((((((((((((((($$l !$d$$$d$$$d$$$d$$((((()) ))&)0)4)9)<)=)D)Y)a)k)o)t)x)y))$$l !$d$$$d$$$d$$$d$$))))))))))))))))) *** *%*(*)*$$l !$d$$$d$$$d$$$d$$* *%*(*W*[*_*b*********+ +++A+E+J+N+}+++++++++++,0,4,9,<,k,o,t,x,,,,,,,,,-!-&-)-X-\-a-d---------. ...D.H.M.P............///3/8/;/j/n/s/y/ CJOJQJCJOJQJnH _)*0*E*M*W*[*_*b*c*j***************$$l !$d$$$d$$$d$$$d$$*****+ +++++/+7+A+E+J+N+O+V+k+s+}+++$d$$$d$$$d$$$d$$$$l !+++++++++++++++++,, ,,&,0,4,$d$$$d$$$d$$$$l !$d$$4,9,<,=,D,Y,a,k,o,t,x,y,,,,,,,,,,,,,$d$$$d$$$$l !$d$$$d$$,,,,,, ---!-&-)-*-1-F-N-X-\-a-d-e-l---$d$$$$l !$d$$$d$$$d$$-----------------. .....2.$$l !$d$$$d$$$d$$$d$$2.:.D.H.M.P.Q.X.m.u...............$$l !$d$$$d$$$d$$$d$$......////%///3/8/;/*CJOJPJQJ CJOJQJCJOJQJnH Bt5u5|5555555555%6slll@dY$$l֞ !$d$$$d$$$d$$$d$$$$l ! %6*6-60666:6C6M6R6X6Y6`6e6i6o6u6o$$ 5 S 3}$d$$u6}66666666666666666666666667$$ 5 S 3}$d$$7 7777!7*7.73747;7@7D7J7P7Y7a7e7j7k7r7w7{77777$$ 5 S 3}$d$$777777777777777777778 88888"8$$ 5 S 3}$d$$"8(8.868>8B8G8H8O8T8X8^8d8l8u8y8~88888888888$$ 5 S 3}$d$$8888888888888889 999 9%9&9-92969<9B9$d$$$$ 5 S 3}B9K9T9X9]9^9e9j9n9t9z999999999999999$$ 5 S 3}$d$$99::::::::":$:%:&:':~|z~||zz&`#$@do$$ 5 S 3}':(:):@d* 00P/ =!"#$%|,,  c yg(,,(d'`* 00P/ =!"#$%|HH?RG(HH(d'`' 0P/ =!"#$%|HH?RG(HH(d'`' 0P/ =!"#$%|HH?RG(HH(d'`'0P= /!"#$%|,, \ J e(,,(d'`$P/ =!"#$%|HH(FG(HH(d'h [4@4NormalCJOJQJkH'mH L@L Heading 1$$d8@&5B*CJOJQJnH L@L Heading 2$$d8@&5B*CJOJQJnH VV Heading 3-$$@d$d%d&d'd@&5:@: Heading 4$@d@&5B@B Heading 5$d@& >*OJQJ<A@<Default Paragraph Font, @,Footer  !,@,Header  !HHtext$ d$5CJOJQJkH'(O"(refld222address$Ih&)@A& Page NumberHS@RHBody Text Indent 3 hOJQJH+@bH Endnote TextH$5$7$8$9D CJOJQJLCrLBody Text Indent $h OJPJQJ8B@8 Body Text pdOJQJ<P@< Body Text 2 ~dOJQJZR@ZBody Text Indent 2$dB*OJQJnH <Q@< Body Text 3 $dOJQJ8Z@8 Plain TextCJOJPJQJPTP Block Text"$$hd "OJQJ)6y\)62,222P3y33444?5e5AA AC     !!! *&A6D-Qaryyx]"M\Q*)6 )~  Y MQ"""""""""""""""""""""""""""%:,!i9q$*y/4):)=OdyBgM.CEQ+fox~e~~.<ɀTn{%6GЇ`m~ '5Iݎcs,9”Sەdv#;ϛXߜau*JТW٣d .D˩Mڪe2?ðP۱m~.<ɷTnw-?ʾϿF8re"4CjG&LyBz 7h3h#M:f)_&RyLd|es$-:FE;JUbb\bV*) m  "   ~%9I+\p0AKK^6  Z!!L""#7$$%;&&':(())**+4,,-2..z/*001.22344t5%6u677"88B99':):      !"#$%&'(*+,-./0123456789:;<>?@ABCDEFGHIJKLMNPQRSTUVWXYZ[\]^_`abcefghijklmnopqrstuvwxz{|}~     ): %!!8@0(  B S  ?)64858X\ n{Z[gTZ~bjI!J!P!!!N"U"$$%%%%%Q'R'[']'e'*$*++++,,------ . ... .00<<L>Q>>>>;@?@@@@@BBCCCdCeCjCCCCDDFFRRCVIV'W-WX%X[XeXXXXXXYUYZYsY|Y]]^ ^j^o^^^^^^^^^^_ ____!_&_'_,_e_k_____v`|```aaaaaabbbcc"c)c0c:cBcxc}cccOdSddd@eDeMeQe[e_eTfXfZf_fqfuf g g;g?gHgLggghhdhhhhhhhdjkjjjjjkkOkTkikpkkk[lelllll m m5m9mCmGmmnnnVn]nknrnsn|nnn oooo1p5pmpqpFqMqlqpq~qqrrrrtttttt uuuuuuuuuuVv[vvvvvvvvvvwzwOxSx_xkx}xx!y%y/y3yByFyzz"z)z.z6zGM8=|żFKͽҽTYپ޾"af.3rw>C JO14vyAD RU _b'*kn"(>D} }  8 @ j q       @I220252M2P26666!6&6'6*6  !9vxt"./:<%0xy ,-8frs~ ,s=JLXcpr~  tvBF>H"1$%%++-=. 114 4*<.<m<q<S=W={>>AAGG~JJVl?lZlttVvqvrvuvOwUwVwnwyy"-!6W`e*/ O T w |       H M y ~     L d     8 < c z        ' E ] l      ,^s3gz 5Oey^b 8J]h126666!6&6'6*6Thomas Brocher2Macintosh HD:Temporary Items:Word Work File A 1294Thomas Brocher?Macintosh HD:SHIPS Experiments:Bellingham SHIPS:OFR:OFR 03-xxxThomas Brocher<Macintosh HD:Temporary Items:AutoRecovery save of OFR 03-xxThomas Brocher?Macintosh HD:SHIPS Experiments:Bellingham SHIPS:OFR:OFR 03-xxxThomas Brocher<Macintosh HD:Temporary Items:AutoRecovery save of OFR 03-xxThomas Brocher<Macintosh HD:Temporary Items:AutoRecovery save of OFR 03-xxThomas Brocher<Macintosh HD:Temporary Items:AutoRecovery save of OFR 03-xxThomas Brocher?Macintosh HD:SHIPS Experiments:Bellingham SHIPS:OFR:OFR 03-xxxThomas BrocherFMacintosh HD:SHIPS Experiments:Bellingham SHIPS:OFR 03-160:OFR 03-160Carolyn Donlin673GB Drive:Work In Progress:OFRs:of03-160:of03-160.txt@#s)6P@GTimes New Roman5Symbol3 Arial3TimesWMTms RmnTimes New Roman5 Geneva? Courier New9New York" ];uf];ufJtf,!!+0d8߱bt&USGS-OFR-98-xxx USGS-OFR-98-xxx Tom BrocherCarolyn Donlin Oh+'0 , H T ` lx''USGS-OFR-98-xxx USGS-OFR-98-xxx SGS Tom Brocherom  of03-160erCarolyn Donlin 2roMicrosoft Word 8.0 @@ܓ@ήJ@ήJ,! ՜.+,D՜.+,h$ hp  'US Geological Surveyx 8: 'USGS-OFR-98-xxx USGS-OFR-98-xxx Title 6> _PID_GUID'AN{7B39B507-5D85-11D4-927F-A2140B0C0AC1}  !"#$%&'()*+,-./0123456789:;<=>?@ABCDEFGHIJKLMNOPQRSTUVWXYZ[\]^_`abcdefghijklmnopqrstuvwxyz{|}~      !"#$%&'()*+,-./0123456789:;<=>?@ABCDEFGHIJKLMNOPQRSTUVWXYZ[\]^_`abcdefghijklmnopqrstuvwxyz{|}~      !"#$%&'()*+,-./012346789:;<>?@ABCDKRoot Entry FzM1Table3WordDocument5SummaryInformation(5DocumentSummaryInformation8=CompObjXObjectPoolzz FMicrosoft Word DocumentNB6WWord.Document.8