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3 edition of Geophysical interpretations west of and within the northwestern part of the Nevada Test Site found in the catalog.

Geophysical interpretations west of and within the northwestern part of the Nevada Test Site

Geophysical interpretations west of and within the northwestern part of the Nevada Test Site

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  • 23 Currently reading

Published by U.S. Geological Survey, Branch of Information Services [distributor] in [Denver, CO] .
Written in English

    Subjects:
  • Gravity -- Nevada -- Nevada Test Site,
  • Groundwater flow -- Nevada -- Nevada Test Site,
  • Geomagnetism -- Nevada -- Nevada Test Site

  • Edition Notes

    Statementby V.J.S. Grauch ... [et al.].
    SeriesOpen-file report -- 97-476., U.S. Geological Survey open-file report -- 97-476.
    ContributionsGrauch, V. J. S., Geological Survey (U.S.)
    The Physical Object
    Paginationiii, 45 p. :
    Number of Pages45
    ID Numbers
    Open LibraryOL17837984M
    OCLC/WorldCa37720529

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Geophysical interpretations west of and within the northwestern part of the Nevada Test Site Download PDF EPUB FB2

@article{osti_, title = {Geophysical interpretations west of and within the northwestern part of the Nevada Test Site}, author = {Grauch, V J and Sawyer, D A and Fridrich, C J and Hudson, M R}, abstractNote = {This report focuses on interpretation of gravity and new magnetic data west of the Nevada Test Site (NTS) and within the northwestern part of NTS.

Get this from a library. Geophysical interpretations west of and within the northwestern part of the Nevada Test Site.

[V J S Grauch; Geological Survey (U.S.);]. This report focuses on interpretation of gravity and new magnetic data west of the Nevada Test Site (NTS) and within the northwestern part of NTS. The interpretations integrate the gravity and magnetic data with other geophysical, geological, and rock property data to put constraints on tectonic and magmatic features not exposed at the surface.

The Pahute Mesa–Oasis Valley region includes the northwestern part of the Nevada Test Site and a contiguous area, of roughly equal size, west of the Test. Geophysical interpretations west of and within the northwestern part of the Nevada Test Site Article 3D/4D MODELLING, VISUALIZATION AND INFORMATION FRAMEWORKS: CURRENT U.S.

GEOLOGICAL SURVEY. A preliminary investigation of the structure of southern Yucca Flat, Massachusetts Mountain, and CP basin, Nevada Test Site, Nevada, based on geophysical modeling.

Maps showing aeromagnetic survey results, locations of gravity station data, and discussions of processing within the report. Info: A Review of Aeromagnetic Anomalies in the Sawatch. Geology of the Yucca Mountain site area, southwestern Nevada Author(s) is an alluviated lowland that slopes gently eastward from an elevation of ∼ m in its northwestern part to m at a low point between Alice and Fran Ridges.

from east to west within the site area, the Paintbrush Canyon, Bow Ridge. A shifting rift—Geophysical insights into the evolution of Rio Grande rift margins and the Embudo transfer zone near Taos, New Mexico From the geophysical interpretations and subsurface models, we infer relations between faulting and flows of Pliocene Servilleta Basalt and older, buried basaltic rocks that, combined with geologic mapping Cited by: 6.

Please note: The following links may contain copyrighted material. Permission has been granted to the National Park Service to post this information online, but the copyrights are still reserved by the owner of the original books.

The Bonneville Salt Flats is located in the west­ ern part of the Great Salt Desert of northwestern Utah (fig. The salt crust on the Bonneville Salt Flats, which covered 43 mi r\ in late summeris unique for its size and accessibility.

The first documented non-Native American explorations of the area were instigated in the earlyCited by: We have made measurements of shear wave splitting in the phases SKS and SKKS at 21 broadband stations in North America, South America, Europe, Asia, and Africa.

Measurements are made using a retrieval scheme that yields the azimuth of the fast polarization direction ϕ and delay time δt of the split shear wave plus uncertainties. Detectable anisotropy was found at. The site characterization, monitoring, and field screening methods covered in the guide are divided into 10 major sections, which are described below.

Because site characterization generally precedes monitoring, earlier sections of the guide tend to cover site characterization methods, while later sections cover monitoring. seismic, gravity, magnetometer, ground penetrating radar, and various borehole methods.

Field investigations to evaluate the application of D.C. resistivity, electromagnetic, self potential and magnetometer methods were undertaken at four. A geologic interpretation of seismic-refraction results in northeastern California G.

FUIS J. ZUCCA* W. MOONEY B. MILKEREIT* or subprovinces, that are arcuate and convex to the west. Within the region of our experiment, these include, from east to west, the eastern Klamath belt, the Trinity ultramafic sheet of Irwin (), the. With an introductory résumé of the progress of geological science within the last two years / (Boston Report on a part of the North west territories drained by the Winisk and Stratigraphy of the unsaturated zone and uppermost part of the Snake River Plain aquifer at test area north, Idaho National Engineering Laboratory.

The measurements of the velocity of compressional waves up to 10 kilobars for some specimens of rock, reported in part 1, are discussed with respect to the effects of porosity, alteration, anisotropy, and composition.

The relations of isotropic elasticity are shown to be approximately valid for a number of examples. Test pits at the Ward Valley site showed macromorphology and features interpreted by Shlemon (Appendix A) as soils or paleosols.

In addition, some of the micromorphologies (pendulous calcite cement at ft. depth, Figure A) are also indicative of pedogenic processes. 1 Introduction [2] Ground penetrating radar (GPR) studies can yield insight into the physical properties, rock‐size distribution, structure, and layering in the shallow subsurface, thereby granting a three‐dimensional view of the processes affecting an area over geologic time.

The broad motivation and implications of the present work relate to how GPR data from terrestrial Cited by: 5. Digital Geologic Map of the Nevada Test Site and Vicinity, Nye, Lincoln, and Clark Counties, Nevada, and Inyo County, California. This digital geologic map of the Nevada Test Site (NTS) and vicinity, as well as its accompanying digital geophysical maps, are compiled atscale.

USGS, DOE, USBM, Engineering, and NBMG Open-File Reports on File at NBMG. These miscellaneous open-file reports are on file in the Information Office of NBMG and are available to the public.

Photocopies can be purchased. For more information contact us by phone at () or via email at [email protected] Aberdeen, E. J., White, W. F., Sherwood, A. M., Bruce, F. L., and Ferguson, D. E.,Interim Report on the Location of Non Saline Uraniferous Waters Suitable for.

The Antevs Library Online Author Title Catalog The catalog includes nearly titles. The following list, arranged alphabetically by first author for dissertations & theses, books and reprints; then by journal, map and media; can be searched using your browser's "FIND" (ctrl-F) utility.

GMC 18 Unknown, [n.d.], Geochemical analysis (total organic carbon, rock-eval, vitrinite reflectance) from the Chevron Kavearak Point #, and Sohio Challenge Island #1 wells, North Slope, Alaska: Alaska Division of Geological & Geophysical Surveys Geologic Materials Center Data Rep 6 p.

PUBLICATIONS OF THE WESTERN GEOLOGIC MAPPING TEAM, Compiled by Paul Stone and Charles L. Powell, II. 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. PART II: REGIONAL GEOPHYSICAL AND GEOLOGICAL CHARACTERISTICS OF Contemporary Stress Orientations Prior Geologic and Tectonic History Paleostress Rotations PART III: REGIONAL INTERPRETATIONS OF BASIN-RANGE TECTONISM GENERAL TECTONIC MODELS i Age of basin and range normal faults in Nevada Test Site and Nellis.

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Dept Characteristics and properties of the basin-fill aquifer determined from three test wells west of Albuquerque, Bernalillo County, New Mexico Nevada Test Site, Nye County, Nevada.

Diachroneity of Basin and Range extension and Yellowstone hotspot volcanism in northwestern Nevada. Geology. 32(2) Locations referred to by this literature: Santa Rosa Range, Humboldt, Nevada.

Colgan, Joseph P., Trevor A. Dumitru, Michael McWilliams, and Elizabeth L. The heterogeneity and complexity of flow paths in fractured rocks make field studies very difficult.

As a result, there are relatively few field study sites where the distribution and character of fractured rocks have been described in detail. These sites are an extremely valuable scientific. Since its first edition, Renfrew and Bahn’s Archaeology: Theories, Methods, and Practice has been the leading academic source on what archaeologists do and how they do it.

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Exposures of interlayered limestone and chert, located west of the Harkless phyllite outcrops, belong to the upper Cambrian Emigrant Formation (e). Stratigraphic sections showing coal correlations within the lower part of the Fort Union Formation in the Baggs area, Carbon County, Wyoming; Stratigraphic sequence measured from Jurassic Todilto limestone to Cretaceous Dakota sandstone, west side of San Juan Basin, near Crystal, San Juan County, New Mexico.

The first and perhaps the most painful part of a project is to define the purpose of the field work; this process will guide the planning stages. Geothermal exploration within volcanic fields has two main goals: (a) identifying and evaluating the heat source and (b) locating permeable zones and the hydrothermal system.

Tomographic V p and V s structure of the California Central Coast Ranges, in the vicinity of SAFOD, from controlled-source seismic data, Geophysical Journal International, VolumeIssue 3, SeptemberPages –, https owing presumably to the fact that the San Andreas fault is located within sedimentary rocks having Cited by: 9.

Hampson, P.S.,Effects of hydraulic borehole mining on ground water at a test site in northeast St. Johns County, Florida: U.S. Geological Survey Water-Resources Investigations Report29 p. Hampson, P.S.,Wetlands in Florida: Tallahassee, Florida Bureau of Geology Geology Map Series1 sheet.

Site 33RO is located south and east of the Square Enclosure in a formerly cultivated field flanked by Paint Creek on the south (Figure 1). The site was originally identified through observation of artifacts on the surface of the field, but relatively little was known about this site and its relationship, if any, to the earthwork complex.

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