Conodont color and surface textural alteration in the Muschelkalk (Triassic) of the Silesian-Cracow Zn-Pb district, Poland
J.E. Repetski, M. Narkiewicz
1996, Prace - Panstwowego Instytutu Geologicznego (154) 112-120
Limestone and dolostone samples were collected from sites within and adjacent to ore zones in the Trzebionka mine, Silesia-Cracow zinc-lead mining district, southern Poland, to assess the level of thermal alteration of the enclosed conodonts, via the color alteration index (CAI) technique, and to study any surface alteration effects on...
Beach-ridge development in Lake Michigan: Shoreline behavior in response to quasi-periodic lake-level events
T.A. Thompson, S.J. Baedke
1996, Marine Geology (129) 163-174
Strandplains of arcuate beach ridges are common in coastal embayments in parts of the Great Lakes. Similarities in beach-ridge development and geomorphology are recognizable in many of the embayments in the Lake Michigan basin despite differences in size and shape, available sediment type and supply, predepositional slope and topography, and...
Water-quality assessment of the Trinity River Basin, Texas - Review and analysis of available pesticide information, 1968-91
R.L. Ulery, M.F. Brown
1995, Water-Resources Investigations Report 94-4218
In 1991 the Trinity River Basin study unit was among the first 20 study units in which work began under full-scale program implementation of the National Water-Quality Assessment Program. A retrospective assessment was undertaken to review and analyze existing pesticide data and related environmental factors. Population and land-use data indicate...
1993 Annual Report: San Francisco estuary regional monitoring program for trace substances
B. Thompson, Jessica Lacy, Dane Hardin, Tom Grovhaug, K. Taberski, Alan D. Jassby, James E. Cloern, J. Caffrey, B. Cole, David H. Schoellhamer
1993, Report
This first annual report of the San Francisco Estuary Regional Monitoring Program contains the results of monitoring measurements made in 1993. Measurements of conventional water quality parameters and trace contaminant concentrations were made at 16 stations throughout the Estuary three times during the year: the wet period (March), during declining...
Reconnaissance data for selected herbicides, two atrazine metabolities, and nitrate in surface water of the Midwestern United States, 1989-90
E.A. Scribner, E.M. Thurman, D. A. Goolsby, M. T. Meyer, M. S. Mills, M.L. Pomes
1993, Open-File Report 93-457
Water-quality data were collected from 147 rivers and streams during 1989-90 to assess selected preemergent herbicides, two atrazine metabolites, and nitrate in 10 Midwestern States. This report includes a description of the sampling design, data collection techniques, laboratory and analytical methods, and a compilation of constituent concentrations and quality-assurance data....
Geologic map of the MTM 25057 and 25052 quadrangles, Kasei Valles region of Mars
David H. Scott
1993, IMAP 2208
Kasei Valles (fig. 1) make up the largest system of outflow channels on Mars and were a major contributor of water to Chryse Planitia. The walls and floors of the Kasei channe<span...
Chronology, Eruption Duration, and Atmospheric Contribution of the Martian Volcano Apollinaris Patera
M.S. Robinson, P. J. Mouginis-Mark, J. R. Zimbelman, S.S.C. Wu, K.K. Ablin, A. E. Howington-Kraus
1993, Icarus (104) 301-323
Geologic mapping, thermal inertia measurements, and an analysis of the color (visual wavelengths) of the martian volcano Apollinaris Patera indicate the existence of two different surface materials, comprising an early, easily eroded edifice, and a more recent, competent fan on the southern flank. A chronology of six major events that...
The Great Ice Age
Louis L. Ray
1992, Report
The Great Ice Age, a recent chapter in the Earth's history, was a period of recurring widespread glaciations. During the Pleistocene Epoch of the geologic time scale, which began about a million or more years ago, mountain glaciers formed on all continents, the icecaps of Antarctica and Greenland were more...
Calibration of the latest Eocene-Oligocene geomagnetic polarity time scale using 40 Ar/ 39 Ar dated ignimbrites
W. C. McIntosh, J. W. Geissman, C.E. Chapin, Michael J. Kunk, Christopher D. Henry
1992, Geology (20) 459-463
A discontinuous record of late Eocene-Oligocene geomagnetic polarity has been determined using high-precision (±<0.15 m.y.) 40Ar/39Ar sanidine dating and a paleomagnetic study of 37-27 Ma ignimbrites in New Mexico, Colorado, and Texas. This record provides age control for several geomagnetic polarity reversals that occurred during three periods of intense ignimbrite volcanism:...
Heat flow and subsurface temperature as evidence for basin-scale ground-water flow, North Slope of Alaska
D. Deming, J.H. Sass, A.H. Lachenbruch, R. F. De Rito
1992, Geological Society of America Bulletin (104) 528-542
In conjunction with the U.S. Geological Survey's exploration program in the National Petroleum Reserve, Alaska (NPRA) several high-resolution temperature logs were made in each of 21 drillholes between 1977 and 1984. These time-series of shallow (average 600-m depth) temperature profiles were extrapolated to...
Regional stratigraphy and subsurface geology of Cenozoic deposits, Gulf Coastal Plain, south-central United States
R.L. Hosman
1991, Open-File Report 91-66
The Gulf Coast Regional Aquifer-System Analysis includes all major aquifer systems in Cenozoic deposits in the Gulf Coastal Plain in the States of Arkansas, Illinois, Kentucky, Louisiana, Mississippi, Missouri, Tennessee, Texas, and small areas in Alabama and Florida (western panhandle area), an area of about 290,000 square miles. The Gulf...
A reinterpretation of the timing, position, and significance of part of the Sacramento Mountains detachment fault, southeastern California
Carol Simpson, Janet Schweitzer, Keith A. Howard
1991, GSA Bulletin (103) 751-761
A contact previously considered to be part of the Sacramento Mountains detachment fault (SDF), exposed in the Sacramento Mountains metamorphic core complex, is reinterpreted as an unconformity between Tertiary rhyolite of Eagle Peak and cataclastically deformed crystalline lower-plate rocks. This reinterpretation is based on outcrop-scale topographic relief and the absence...
Geohydrology of the alluvial and terrace deposits of the North Canadian River from Oklahoma City to Eufaula Lake, central Oklahoma
J.S. Havens
1989, Water-Resources Investigations Report 88-4234
This investigation was undertaken to describe the geohydrology of the alluvial and terrace deposits along the North Canadian River between Lake Overholser and Eufaula Lake, an area of about 1,835 square miles, and to determine the maximum annual yield of ground water. A 1982 water-level map of the alluvial and terrace...
National water summary 1986: Hydrologic events and ground-water quality
United States Geological Survey
1988, Water Supply Paper 2325
Ground water is one of the most important natural resources of the United States and degradation of its quality could have a major effect on the welfare of the Nation. Currently (1985), ground water is the source of drinking water for 53 percent of the Nation's population and for more...
Morphometric variability within the axial zone of the southern Juan de Fuca Ridge: Interpretation from Sea MARC II, Sea MARC I, and deep-sea photography
Ellen S. Kappel, William R. Normark
1987, Journal of Geophysical Research B: Solid Earth (92) 11291-11302
The morphometric characteristics of the axial regions of oceanic spreading centers are determined by (1) the type of volcanic flows, (2) the relation between primary volcanic relief (on a scale of a few meters to tens of meters) and degree of sediment cover, and (3) the extent of surficial expression...
Thermal evolution of a differentiated Ganymede and implications for surface features
Randolph L. Kirk, David J. Stevenson
1987, Icarus (69) 91-134
Thermal evolution models are presented for Ganymede, assuming a mostly differentiated initial state of a water ocean overlying a rock layer. The only heat sources are assumed to be primordial heat (provided by accretion) and the long-lived radiogenic heat sources in the rock component. As Ganymede cools, the ocean thins,...
Identification and description of potential ground-water quality monitoring wells in Florida
P. R. Seaber, M.E. Thagard
1986, Water-Resources Investigations Report 85-4130
The results of a survey of existing wells in Florida that meet the following criteria are presented: (1) well location is known , (2) principal aquifer is known, (3) depth of well is known, (4) well casing depth is known, (5) well water had been analyzed between 1970 and 1982,...
Ground-water flow in low permeability environments
Christopher E. Neuzil
1986, Water Resources Research (22) 1163-1195
Certain geologic media are known to have small permeability; subsurface environments composed of these media and lacking well developed secondary permeability have groundwater flow sytems with many distinctive characteristics. Moreover, groundwater flow in these environments appears to influence the evolution of certain hydrologic, geologic, and geochemical systems, may affect the...
Technical problems in the construction of a map to zone the earthquake ground-shaking hazard in the United States
W. W. Hays
1984, Engineering Geology (20) 13-23
Zoning of the earthquake ground-shaking hazard — the division of a region into geographic areas having a similar relative severity or response to ground shaking — has been a goal in the United States for about fifty years. During this period,...
Index of faults of Cretaceous and Cenozoic age in the eastern United States
David C. Prowell
1983, Miscellaneous Field Studies Map 1269
The information in this report was collected between 1974 and 1982 as part of the Reactor Hazards Program of the U.S. Geological Survey (USGS). This program was initiated to delineate and assess geologic hazards that could be particularly detrimental to major constructions, especially nuclear reactors. Faults are of principal interest...
The ophiolitic North Fork terrane in the Salmon River region, central Klamath Mountains, California
C.J. Ando, W. P. Irwin, D. L. Jones, J.B. Saleeby
1983, GSA Bulletin (94) 236-252
The North Fork terrane is an assemblage of ophiolitic and other oceanic volcanic and sedimentary rocks that has been internally imbricated and folded. The ophiolitic rocks form a north-trending belt through the central part of the region and consist of a disrupted sequence of homogeneous gabbro, diabase, massive to pillowed...
The past is the key to the future
B. R. Doe
1983, Geochimica et Cosmochimica Acta (47) 1341-1354
A new major frontier of geological research, which was initiated in the 1970's, involves predicting future geologic trends or events through study of the present and past, rather than trying to understand the past, often using what one knows about the present. Like most scientific frontiers, this one began from...
A model for managing sources of groundwater pollution
Steven M. Gorelick
1982, Water Resources Research (18) 773-781
The waste disposal capacity of a groundwater system can be maximized while maintaining water quality at specified locations by using a groundwater pollutant source management model that is based upon linear programing and numerical simulation. The decision variables of the management model are solute waste disposal rates at various facilities...
U-Pb isotope systematics and age of uranium mineralization, Midnite mine, Washington.
K.R. Ludwig, J. T. Nash, C. W. Naeser
1981, Economic Geology (76) 89-110
Uranium ores at the Midnite mine, near Spokane, Washington, occur in phyllites and calcsilicates of the Proterozoic Togo Formation, near the margins of an anomalously uraniferous, porphyritic quartz monzonite of Late Cretaceous age. The present geometry of the ore zones is tabular, with the thickest zones above depressions in the...
A lithologic-tectonic framework for the metallogenic provinces of California
J. P. Albers
1981, Economic Geology (76) 765-790
The lithologic-tectonic framework of California developed principally during Mesozoic time when various terranes of oceanic crust and island-arc crust were accreted to older sialic crust, resulting in westward growth of the continent. Emplacement of great batholithic masses of granitoid rocks cutting all these crustal types also took place during the...