<?xml version="1.0" encoding="ISO-8859-1"?>
<metadata>
<idinfo>
<citation>
<citeinfo>
<origin>Eric Grossman</origin>
<origin>Patrick E. Hart</origin>
<origin>Michael E. Field</origin>
<origin>Peter Triezenberg</origin>
<pubdate>2006</pubdate>
<title>
High-resolution chirp seismic-reflection data acquired from the
Cap de Creus shelf and canyon area, Gulf of Lions, Spain in 2004
</title>
<geoform>seismic reflection profile section</geoform>
<serinfo>
<sername>U.S. Geological Survey Open-File Report</sername>
<issue>2006-1247</issue>
</serinfo>
<pubinfo>
<pubplace>Menlo Park, CA</pubplace>
<publish>U.S. Geological Survey</publish>
</pubinfo>
<onlink>&lt;http://pubs.usgs.gov/of/2006/1247/&gt;</onlink>
</citeinfo>
</citation>
<descript>
<abstract>
This report consists of high-resolution chirp seismic reflection profile
data from the northern Gulf of Lions, Spain. These data were acquired in
2004 using the Research Vessel Oceanus (USGS Cruise ID: O-1-04-MS). The
data are available in binary and JPEG image formats. Binary data are
in Society of Exploration Geologists (SEG) SEG-Y format and may be
downloaded for further processing or display. Reference maps and
JPEG images of the profiles may be viewed with your Web browser.
</abstract>
<purpose>
Marine seismic reflection data are used to image and map
sedimentary and structural features of the seafloor and subsurface.
These data were acquired across the shelf and canyon area of the Gulf
of Lions, Spain as part of a multinational effort to characterize the
geologic framework and sedimentary environment of the region.
The specific objective of this seismic survey is to provide seismic
reflection images of the depositional geometry of the upper 50 meters of
subbottom stratigraphy in order to better understand the mechanisms of
sediment transport and deposition. These chirp seismic profiles provide
high-quality images with approximately 20 cm of vertical
resolution and up to 80 m of subbottom penetration.
</purpose>
<supplinf>
Chirp seismic reflection profiles are acquired by means of an
acoustic source and a hydrophone array, both contained in a single unit
towed in the water behind a survey vessel. The sound source emits a
short (30 ms) swept-frequency (500 to 7200 Hz)acoustic pulse,
which propagates through the water and sediment columns. The acoustic
energy is reflected at density boundaries (such as the seafloor or
sediment layers beneath the seafloor), and detected by the hydrophone
array, and digitally recorded by the onboard PC-based acquisition system.
As the vessel moves, this process is repeated multiple times per second,
producing a two-dimensional image of the shallow geologic structure
beneath the ship track.
Additional information about the USGS survey O-1-04-MS is available at
&lt;http://walrus.wr.usgs.gov/infobank/o/o104ms/html/o-1-04-ms.meta.html&gt;.
</supplinf>
</descript>
<timeperd>
<timeinfo>
<rngdates>
<begdate>20030925</begdate>
<enddate>20031001</enddate>
</rngdates>
</timeinfo>
<current>
Data assumed to be constant over time, but the imaged geology may
change due to geologic processes.
</current>
</timeperd>
<status>
<progress>Complete</progress>
<update>None planned</update>
</status>
<spdom>
<bounding>
<westbc>3.1808</westbc>
<eastbc>3.4586</eastbc>
<northbc>42.4418</northbc>
<southbc>42.1763</southbc>
</bounding>
</spdom>
<keywords>
<theme>
<themekt>General</themekt>
<themekey>U.S. Geological Survey</themekey>
<themekey>USGS</themekey>
<themekey>Coastal and Marine Geology Program</themekey>
<themekey>CMGP</themekey>
<themekey>EuroSTRATAFORM</themekey>
<themekey>Seismic Reflection</themekey>
<themekey>Sedimentation</themekey>
</theme>
<theme>
<themekt>ISO 19115 Topic Category</themekt>
<themekey>geoscientificinformation</themekey>
<themekey>imageryBaseMapsEarthCover</themekey>
<themekey>oceans</themekey>
</theme>
<place>
<placekt>General</placekt>
<placekey>Cap de Creus Shelf</placekey>
<placekey>Cap de Creus Canyon</placekey>
<placekey>Gulf of Lions</placekey>
<placekey>Spain</placekey>
</place>
<place>
<placekt>Geographic Names Information System (GNIS)</placekt>
<placekey>Mediterranean Sea</placekey>
</place>
</keywords>
<accconst>None. These data are held in the public domain.</accconst>
<useconst>
The U.S. Geological Survey requests to be acknowledged as the originator
of the data in future products or derivative research.
</useconst>
<ptcontac>
<cntinfo>
<cntperp>
<cntper>Eric Grossman</cntper>
<cntorg>U.S. Geological Survey</cntorg>
</cntperp>
<cntpos>Geologist</cntpos>
<cntaddr>
<addrtype>mailing address</addrtype>
<address>400 Natural Bridges Drive</address>
<city>Santa Cruz</city>
<state>CA</state>
<postal>95060-5792</postal>
<country>USA</country>
</cntaddr>
<cntvoice>831-427-4725</cntvoice>
<cntemail>egrossman@usgs.gov</cntemail>
</cntinfo>
</ptcontac>
<browse>
<browsen>&lt;http://pubs.usgs.gov/of/2006/1247/images/gol_coverage_area.png&gt;</browsen>
<browsed>Map of Gulf of Lions showing areas of 2004 USGS chirp seismic refleciton research cruise</browsed>
<browset>PNG</browset>
</browse>
<crossref>
<citeinfo>
<origin>Alonso, B.</origin>
<origin>Canals, M.</origin>
<origin>Got, H.</origin>
<origin>Maldonado, A.</origin>
<pubdate>1991</pubdate>
<title>
Sea valleys and related depositional systems in the Gulf of
Lions and Ebro continental margin
</title>
<serinfo>
<sername>American Association of Petroleum Geologists Bulletin</sername>
<issue>75, p. 1195-1214</issue>
</serinfo>
<pubinfo>
<pubplace>Tulsa, OK</pubplace>
<publish>American Association of Petroleum Geologists</publish>
</pubinfo>
</citeinfo>
</crossref>
<crossref>
<citeinfo>
<origin>Baztan, J.</origin>
<origin>Berné, S.,</origin>
<origin>Olivet, J.-L</origin>
<origin>Rabineau, M.</origin>
<origin>Aslanian, D.</origin>
<origin>Gaudin, M.</origin>
<origin>Réhault, J.P.</origin>
<origin>Canals, M.</origin>
<pubdate>2005</pubdate>
<title>
The axial incision: the key to understand canyon evolution (in
the western Gulf of Lions)
</title>
<serinfo>
<sername>Marine and Petroleum Geology</sername>
<issue>22, n. 6-7, p. 805-826</issue>
</serinfo>
<pubinfo>
<pubplace>Guildford, Surrey, England</pubplace>
<publish>Butterworth Scientific Ltd.</publish>
</pubinfo>
</citeinfo>
</crossref>
<crossref>
<citeinfo>
<origin>Berné, S.</origin>
<origin>Carré, D.</origin>
<origin>Loubrieu, B.</origin>
<origin>Mazé, J.-P.</origin>
<origin>Normand, A.</origin>
<pubdate>2001</pubdate>
<title>Carte morphobathymétrique du Golfe du Lion à l’ échelle 1/100 000 éme</title>
<pubinfo>
<pubplace>Brest, France</pubplace>
<publish>Ifremer, Brest</publish>
</pubinfo>
</citeinfo>
</crossref>
<crossref>
<citeinfo>
<origin>Berné, S.</origin>
<origin>Gorini, C.</origin>
<pubdate>2005</pubdate>
<title>
The Gulf of Lions: An overview of recent studies within the
French Margins’ Programme
</title>
<serinfo>
<sername>Marine and Petroleum Geology</sername>
<issue>22, n. 6-7, p. 691-693</issue>
</serinfo>
<pubinfo>
<pubplace>Guildford, Surrey, England</pubplace>
<publish>Butterworth Scientific Ltd.</publish>
</pubinfo>
</citeinfo>
</crossref>
<crossref>
<citeinfo>
<origin>Berné, S.</origin>
<origin>Carré, B.</origin>
<origin>Loubrieu, B.</origin>
<origin>Mazé, J.P.</origin>
<origin>Morvan, L.</origin>
<origin>Normand, A.</origin>
<pubdate>2004</pubdate>
<title>Le Golfe du Lion. Carte morpho-bathymétrique</title>
<pubinfo>
<pubplace>Brest, France</pubplace>
<publish>Ifremer, Brest</publish>
</pubinfo>
</citeinfo>
</crossref>
<crossref>
<citeinfo>
<origin>Berné, S.</origin>
<origin>Loubrieu, B.</origin>
<origin>The Calmar scientific party</origin>
<pubdate>1999</pubdate>
<title>
Canyons and recent sedimentary processes on the western
Gulf of Lions margin
</title>
<serinfo>
<sername>First results of the Calmar cruise. Comptes Rendus de l&apos;Académie des Sciences de Paris</sername>
<issue>328: 471-477</issue>
</serinfo>
<pubinfo>
<pubplace>Paris</pubplace>
<publish>l&apos;Académie des Sciences de Paris</publish>
</pubinfo>
</citeinfo>
</crossref>
<crossref>
<citeinfo>
<origin>Berné, S.</origin>
<origin>Loubrieu, B.</origin>
<origin>l’équipe embarquée CALMAR</origin>
<pubdate>1997</pubdate>
<title>
Carte morpho-bathymetrie de la marge occidentale du Golfe
du Lion à l’ échelle 1/250 000 éme
</title>
<pubinfo>
<pubplace>Brest, France</pubplace>
<publish>Ifremer, Brest</publish>
</pubinfo>
</citeinfo>
</crossref>
<crossref>
<citeinfo>
<origin>Correggiari, A.</origin>
<origin>Trincardi, F.</origin>
<origin>Langone, L.</origin>
<origin>Roveri, M.</origin>
<pubdate>2001</pubdate>
<title>
Styles of failure in Late Holocene highstand prodelta
wedges on the Adriatic shelf
</title>
<serinfo>
<sername>Journal of Sedimentary Geology</sername>
<issue>71, p. 218-236</issue>
</serinfo>
<pubinfo>
<pubplace>Tulsa, OK</pubplace>
<publish>SEPM (Society for Sedimentary Geology)</publish>
</pubinfo>
</citeinfo>
</crossref>
<crossref>
<citeinfo>
<origin>Grossman, E.E.</origin>
<origin>Hart, P.</origin>
<origin>Field, M.E.</origin>
<pubdate>2005</pubdate>
<title>
Evidence of recent sediment storage and transport
from shallow seismic stratigraphy on the Cap de Creus shelf, Spain
</title>
<serinfo>
<sername>EuroSTRATAFORM - Promess Joint Meeting, Salamanca, Spain, October 24-27, 2005</sername>
<issue>October 24-27, 2005</issue>
</serinfo>
<othercit>&lt;http://www.soc.soton.ac.uk/CHD/EUROSTRATAFORM/salamanca2005/index.html&gt;</othercit>
</citeinfo>
</crossref>
<crossref>
<citeinfo>
<origin>Lofi, J.</origin>
<origin>Rabineau, M.</origin>
<origin>Gorini, C.</origin>
<origin>Berne, S.</origin>
<origin>Clauzon, G.</origin>
<origin>De Clarens, P.</origin>
<origin>Tadeu Dos Reis, A.</origin>
<origin>Mountain, G.S.</origin>
<origin>Ryan, W.B.F.</origin>
<origin>Steckler, M.S.</origin>
<origin>Fouchet, C.</origin>
<pubdate>2003</pubdate>
<title>
Plio-Quaternary prograding clinoform wedges of the
western Gulf of Lion continental margin (NW Mediterranean)
after the Messinian Salinity Crisis
</title>
<serinfo>
<sername>Marine Geology</sername>
<issue>198(3-4): 289-317</issue>
</serinfo>
<pubinfo>
<pubplace>Amsterdam</pubplace>
<publish>Elsevier Scientific Pub. Co</publish>
</pubinfo>
</citeinfo>
</crossref>
<crossref>
<citeinfo>
<origin>Marsset, T.</origin>
<origin>Bellec, V.</origin>
<pubdate>2002</pubdate>
<title>
Late Pleistocene-Holocene deposits on the Rhone inner
continental shelf (France): detailed mapping and
correlation with previous continental and marine studies
</title>
<serinfo>
<sername>Sedimentology</sername>
<issue>49, p. 255-276</issue>
</serinfo>
<pubinfo>
<pubplace>Blackwell Scientific Publishers</pubplace>
<publish>Oxford, Boston</publish>
</pubinfo>
</citeinfo>
</crossref>
<crossref>
<citeinfo>
<origin>Rabineau, M.</origin>
<origin>Berné, S.</origin>
<origin>Le Drezen, E.</origin>
<origin>Lericolais, G.</origin>
<origin>Rutunno, M.</origin>
<pubdate>1998</pubdate>
<title>
3D architecture of lowstand and transgressive Quaternary
sand bodies on the outer shelf of the Gulf of Lions, France
</title>
<serinfo>
<sername>Marine Petroleum Geology</sername>
<issue>15, p. 439-452</issue>
</serinfo>
<pubinfo>
<pubplace>Guildford, Surrey, England</pubplace>
<publish>Butterworth Scientific Ltd.</publish>
</pubinfo>
</citeinfo>
</crossref>
<crossref>
<citeinfo>
<origin>Rabineau, M.</origin>
<origin>Berné, S.</origin>
<origin>Aslanian, D.</origin>
<origin>Olivet, J.-L.</origin>
<origin>Phillipe, J.</origin>
<origin>Guillocheau, F.</origin>
<origin>Bourillet, J.-F.</origin>
<origin>Ledrezen, E.</origin>
<origin>Granjeon, D.</origin>
<pubdate>2005</pubdate>
<title>
Sedimentary sequences in the Gulf of Lions: a record of
100,000 years climatic cycles
</title>
<serinfo>
<sername>Marine and Petroleum Geology</sername>
<issue>22, n. 607, p. 775-804</issue>
</serinfo>
<pubinfo>
<pubplace>Guildford, Surrey, England</pubplace>
<publish>Butterworth Scientific Ltd.</publish>
</pubinfo>
</citeinfo>
</crossref>
<crossref>
<citeinfo>
<origin>Schoolmeester, T.</origin>
<origin>Grossman, E.E.</origin>
<origin>García-García, A.</origin>
<origin>Canals, M.</origin>
<origin>Field, M.</origin>
<origin>Levey, M.</origin>
<origin>Fabres, J.</origin>
<origin>Orange, D.</origin>
<pubdate>2005</pubdate>
<title>
Shallow Sediment Structure revealed from High Resolution
Surveys in the Upper Cap de Creus Canyon
</title>
<serinfo>
<sername>EuroSTRATAFORM - Promess Joint Meeting, Salamanca, Spain, October 24-27, 2005</sername>
<issue>October 24-27, 2005</issue>
</serinfo>
<othercit>&lt;http://www.soc.soton.ac.uk/CHD/EUROSTRATAFORM/salamanca2005/index.html&gt;</othercit>
</citeinfo>
</crossref>
<crossref>
<citeinfo>
<origin>Torres, J.</origin>
<origin>Savoye, B.</origin>
<origin>Cochonat, P.</origin>
<pubdate>1995</pubdate>
<title>
The effects of sea level changes on the Rhone slope
sedimentation (northwestern Mediterranean) as indicated by seismic stratigraphy
</title>
<serinfo>
<sername>Journal of Sedimentary Research</sername>
<issue>65, p. 368-38</issue>
</serinfo>
<pubinfo>
<pubplace>Tulsa, OK</pubplace>
<publish>SEPM (Society for Sedimentary Geology)</publish>
</pubinfo>
</citeinfo>
</crossref>
</idinfo>
<dataqual>
<attracc>
<attraccr>
The validity or accuracy of marine seismic reflection profiles is
highly qualitative, and depends on equipment and operating condition
variables too numerous to quantify. There have been no efforts to
assess the validity of the data.
</attraccr>
</attracc>
<logic>These data have not been assessed for internal consistency.</logic>
<complete>
These are sparse line coverages (2D).
Therefore, data are inherently incomplete. Geologic details between
lines must be inferred. The surveys were not designed to cover a
particular geographic area; the line spacings and azimuths were chosen
to assess the regional stratigraphy.
</complete>
<posacc>
<horizpa>
<horizpar>
Positions were determined with
differential Global Positioning System (GPS). Absolute position
accuracy was approximately plus/minus 10 m.
</horizpar>
</horizpa>
<vertacc>
<vertaccr>
The vertical position was local sea level and there have been no
corrections to a datum or for tidal variations.
</vertaccr>
</vertacc>
</posacc>
<lineage>
<procstep>
<procdesc>
Single-channel chirp seismic reflection data were acquired using an
Edgetech 512i subbottom profiling system.  This &quot;fish &quot; was towed aft
of the research vessel at a depth of approximately 15 meters at a
ship speed of approximately 4 knots. A 30 ms swept-frequency
(500 to 7200 Hz)&quot;chirp&quot; source signal was emitted 1 to 4 times
per second depending on water depth and the returning reflections
were detected by hydrophones located along the bottom of the fish.
The data were digitally recorded by an on-board PC-based Delph Seismic
recording system. Differential GPS position fixes were written into
the seismic data trace headers and are also available in an ASCII
text file.
</procdesc>
<procdate>2004</procdate>
</procstep>
<procstep>
<procdesc>
Open File preparation: The seismic profiles were converted from
Delph Seimic proprietary format to standard SEG-Y format and to
CGM plot files using Paradigm Focus software. Then the CGM files were
converted to 300 dots per inch JPEG image file using Larson CGM to
Image software.  The SEG-Y data files and the JPEG image files are
available for download from this on-line report.
</procdesc>
<procdate>2004</procdate>
<proccont>
<cntinfo>
<cntperp>
<cntper>Patrick E. Hart</cntper>
<cntorg>U.S. Geological Survey</cntorg>
</cntperp>
<cntpos>Geophysicist</cntpos>
<cntaddr>
<addrtype>mailing address</addrtype>
<address>345 Middlefield Road Mail Stop 999</address>
<city>Menlo Park</city>
<state>CA</state>
<postal>94025-3561</postal>
<country>USA</country>
</cntaddr>
<cntvoice>650-329-5160</cntvoice>
<cntemail>hart@usgs.gov</cntemail>
</cntinfo>
</proccont>
</procstep>
</lineage>
</dataqual>
<spdoinfo>
<indspref>
Horizontal X and Y locations for the seimic profiles location are provided
in ASCII position files and are alos stored in the SEG-Y data trace headers
in the standard header locations.
</indspref>
</spdoinfo>
<spref>
<horizsys>
<geograph>
<latres>0.00001</latres>
<longres>0.00001</longres>
<geogunit>decimal degrees</geogunit>
</geograph>
<geodetic>
<horizdn>WGS 84</horizdn>
<ellips>WGS 84</ellips>
<semiaxis>6378137 m</semiaxis>
<denflat>298.257</denflat>
</geodetic>
</horizsys>
</spref>
<eainfo>
<overview>
<eaover>
Binary data file: Each profile is
available as a binary file in Society of Exploration Geophysicists
SEG-Y format. A SEG-Y file consists of 1) a 3200-byte file
identification record of EBCDIC encoded general information; 2) a
400-byte binary record with information such as sample rate and
record length specific to the data set; and 3) multiple records, one
seismic reflection trace per record. Each trace record is preceded
by a 240-byte &quot;trace header&quot; containing information such as trace
number and acquisition day and time specific to each trace. The
trace data are represented as a time series of unitless 16-bit
integer or 32-bit real numbers proportional to the pressure recorded
at each hydrophone. The SEG-Y file is useful only if you have access
to specialized software designed to process and display seismic
reflection data.
</eaover>
<eaover>
Graphic image file: Each profile is
available as a JPEG image.
</eaover>
<eadetcit>
Barry, K.M., Cavers, D.A., and
Kneale, C.W., 1975, Recommended standards for digital tape formats:
Geophysics, v. 40, n. 2, p. 344 - 352. Also available online at:
&lt;http://www.seg.org/publications/tech-stand/&gt;
</eadetcit>
</overview>
</eainfo>
<distinfo>
<distrib>
<cntinfo>
<cntperp>
<cntper>Eric Grossman</cntper>
<cntorg>U.S. Geological Survey</cntorg>
</cntperp>
<cntpos>Geologist</cntpos>
<cntaddr>
<addrtype>mailing address</addrtype>
<address>USGS, 400 Natural Bridges Drive</address>
<city>Santa Cruz</city>
<state>CA</state>
<postal>95060-5792</postal>
<country>USA</country>
</cntaddr>
<cntvoice>831-427-4725</cntvoice>
<cntemail>egrossman@usgs.gov</cntemail>
<cntinst>
Data may be available off-line only by special
arrangement with the distributor above. Please use the on-line
download option unless precluded by download times or access
difficulties.
</cntinst>
</cntinfo>
</distrib>
<resdesc>U.S. Geological Suvey Open-File Report 2006-1247</resdesc>
<distliab>
This dataset was prepared by an agency of the
United States Government. Neither the United States Government nor any
agency thereof nor any of their employees, make any warranty, expressed
or implied, or assumes any legal liability or responsibility for
information, apparatus, products, or processes disclosed in this
report, nor represents that its use would not infringe privately owned
rights. Reference herein to any specific commercial product, process,
or service by trade name, trademark, manufacturer, or otherwise does
not constitute or imply its endorsement, recommendation, or favoring
by the United States Government or any agency thereof.
Although all data published in this report have been used by the USGS,
no warranty, expressed or implied, is made by the USGS as to the
accuracy of the data and related materials. The act of distribution
shall not constitute any such warranty, and no responsibility is
assumed by the USGS in the use of this data.
</distliab>
<stdorder>
<digform>
<digtinfo>
<formname>SEG-Y, JPEG, ASCII</formname>
<transize>2.5 gigabytes</transize>
</digtinfo>
<digtopt>
<onlinopt>
<computer>
<networka>
<networkr>&lt;http://pubs.usgs.gov/of/2006/1247/&gt;</networkr>
</networka>
</computer>
</onlinopt>
<offoptn>
<offmedia>CD-R or DVD-R</offmedia>
<recfmt>ISO 9660</recfmt>
</offoptn>
</digtopt>
</digform>
<fees>none</fees>
</stdorder>
<techpreq>
Use of SEG-Y data requires specialized software,
such as ProMax and Seisworks by Landmark Geophysical; FOCUS and SeisX
by Paradigm Geophysical; SPW by Parallel Geoscience; or VISTA by
Seismic Image Software.
</techpreq>
</distinfo>
<metainfo>
<metd>20060728</metd>
<metc>
<cntinfo>
<cntperp>
<cntper>Eric Grossman</cntper>
<cntorg>U.S. Geological Survey</cntorg>
</cntperp>
<cntpos>Geologist</cntpos>
<cntaddr>
<addrtype>mailing address</addrtype>
<address>USGS, 400 Natural Bridges Drive</address>
<city>Santa Cruz</city>
<state>CA</state>
<postal>95060-5792</postal>
<country>USA</country>
</cntaddr>
<cntvoice>831-427-4725</cntvoice>
<cntemail>egrossman@usgs.gov</cntemail>
</cntinfo>
</metc>
<metstdn>Content Standard for Digital Geospatial Metadata</metstdn>
<metstdv>FGDC-STD-001-1998</metstdv>
</metainfo>
</metadata>

