1961
DOI: 10.3133/ofr6119
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Geologic map of Oak Spring quadrangle, Nye County, Nevada

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Cited by 25 publications
(41 citation statements)
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“…The northernmost vestige of the CP thrust system within the Yucca Flat area is interpreted from relations preserved in the contact aureole of the Cretaceous Climax stock. Micaceous quartzites that most likely belong to the Late Proterozoic Wood Canyon Formation are exposed southeast of calc-silicate gneisses that are correlated with the Ordovician Pogonip Group (Houser and Poole, 1960;Barnes, Houser, and Poole, 1963). This relationship indicates vergence toward the northwest, consistent with CP thrust kinematics.…”
Section: Syncline Ridge and Northwestern Yucca Flatmentioning
confidence: 52%
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“…The northernmost vestige of the CP thrust system within the Yucca Flat area is interpreted from relations preserved in the contact aureole of the Cretaceous Climax stock. Micaceous quartzites that most likely belong to the Late Proterozoic Wood Canyon Formation are exposed southeast of calc-silicate gneisses that are correlated with the Ordovician Pogonip Group (Houser and Poole, 1960;Barnes, Houser, and Poole, 1963). This relationship indicates vergence toward the northwest, consistent with CP thrust kinematics.…”
Section: Syncline Ridge and Northwestern Yucca Flatmentioning
confidence: 52%
“…Our understanding of the geology in the Climax stock area reflects considerable new mapping by Cole, results of our stratigraphic and structural studies (Trexler and others, 1996), and additional paleontologic work by Harris. Prior geologic maps by Houser and Poole (1960), Barnes, Houser, and Poole (1963), and Sargent and Orkild (1973) provided a useful regional guide for our more recent detailed work.…”
Section: Carbonate Wash and The Oak Spring Areamentioning
confidence: 99%
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“…During Precambrian and Paleozoic time, as much as 10,000 meters (m) (32,800 feet [ft]) of marine sediments were deposited in the NNSS region (Cole, 1997). The only surface exposure of Mesozoicage rocks in the NNSS area are granitic intrusive masses, the Gold Meadows Stock north of Rainier Mesa (Gibbons et al, 1963;Snyder, 1977), and the Climax Stock located at the extreme north end of Yucca Flat (Barnes et al, 1963;Maldonado, 1977) ( …”
Section: Att A-2mentioning
confidence: 99%
“…During Precambrian and Paleozoic time, as much as 10,000 m (32,800 ft) of marine sediments were deposited in the NTS region (Cole, 1997). The only surface exposure of Mesozoic-age rocks in the NTS area are granitic intrusive masses, the Gold Meadows Stock north of Rainier Mesa (Snyder, 1977;Gibbons et al,1963 ), and the Climax Stock located at the extreme north end of Yucca Flat (Maldonado, 1977;Barnes et al, 1963) (Figure A-5). Wahl et al (1997) andFerguson et al (1994).…”
Section: A41 Geologic Settingmentioning
confidence: 99%