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Emigrant Trail-Bradley

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Journal Article
Journal: AAPG Bulletin
Published: 01 April 1984
AAPG Bulletin (1984) 68 (4): 504.
...-displaced Emigrant Trail-Bradley Peak-Shirley thrust complex, were crumpled into anticlinal folds such as O’Brien Springs and Horseshoe Ridge. Oil and gas ranging in age from Pennsylvanian to Upper Cretaceous have been found in these structures. Only 7 wells have been drilled in the deeper part of the Hanna...
Image
Geologic Map of the Ferris Mountains – Bear Mountain field area ( a ) and c...
Published: 11 December 2006
and incorporates all the units shaded in light gray. The eastern Ferris Mountains is characterized by interference between north-vergent and south-vergent Laramide thrust faults. Phanerozoic units within the footwall of the south-vergent Emigrant TrailBradley Peak (ET–BP) thrust fault are completely overturned
Image
Geologic Map of the Ferris Mountains – Bear Mountain field area ( a ) and c...
Published: 11 December 2006
and incorporates all the units shaded in light gray. The eastern Ferris Mountains is characterized by interference between north-vergent and south-vergent Laramide thrust faults. Phanerozoic units within the footwall of the south-vergent Emigrant TrailBradley Peak (ET–BP) thrust fault are completely overturned
Journal Article
Published: 11 December 2006
Canadian Journal of Earth Sciences (2006) 43 (10): 1467–1487.
... and incorporates all the units shaded in light gray. The eastern Ferris Mountains is characterized by interference between north-vergent and south-vergent Laramide thrust faults. Phanerozoic units within the footwall of the south-vergent Emigrant TrailBradley Peak (ET–BP) thrust fault are completely overturned...
FIGURES | View All (19)
Journal Article
Journal: PALAIOS
Published: 01 January 2010
PALAIOS (2010) 25 (4): 247–259.
... a ∼40 km 2 region remains temporally uniform over a 5.4 myr interval of time recorded by the Pinery, Rader, Lamar, and Reef Trail Members of the middle Permian (Capitanian) Bell Canyon Formation (BCF). Two third-order sequence boundaries have been previously recognized in this formation, indicating...
FIGURES | View All (9)
Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 20 December 2018
Lithosphere (2019) 11 (1): 129–148.
... of deformation in Wyoming ( Fig. 1 ). Other less significant thrusts with a NNW orientation include the Rio, Emigrant Trail, Casper Arch, and Seminoe thrusts. The major thrusts are the thick-skinned, basement-involved, Laramide structures, with dips of 30°–45° at the surface ( Smithson et al., 1979 ; Stone...
FIGURES | View All (14)
Journal Article
Journal: AAPG Bulletin
Published: 01 January 1976
AAPG Bulletin (1976) 60 (1): 12–33.
... anticline which is essentially barren of petroleum although it is the lowest structurally and best defined topographically of the three anticlines. The three anticlines lie south of, and en echelon to, an east-trending zone of reverse faults that includes the Emigrant Trail thrust ( Figs. 1 , 2 ) near...
FIGURES | View All (11)
Journal Article
Published: 01 January 2014
Rocky Mountain Geology (2014) 49 (2): 191–199.
... in the library or visit many of his associates, including N. H. Darton, who, at that time, was a small, wizened old man about the same age as I am now. Particular treats were visits with Jewel Glass and Taisia Stadnichenko. Miss Stadnichenko was a coal geochemist who emigrated to the U.S. during the Russian...
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Series: Geological Society, London, Special Publications
Published: 01 January 2019
DOI: 10.1144/SP480.12
EISBN: 9781786204240
... and, in the afternoon on their way back through the forest, they lost the trail. Geikie mentions that he first noticed that Dan was leading them far towards the right into a forest that was getting darker every minute. At first Dan did not admit it, but eventually he consented and turned to the left. But night...
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Series: GSA Field Guide
Published: 01 January 2011
DOI: 10.1130/2011.0021(06)
EISBN: 9780813756219
.... Occupying the center of the basin in the shape of a large, irregular lens ( Bradley, 1964 ; Roehler, 1992b , 1993 ), the Green River Formation is the result of at least five million years of lacustrine deposition lasting from ca. 53.5 to 48.5 Ma ( Smith et al., 2003 ), although lacustrine deposition may...
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Journal Article
Journal: Geosphere
Published: 22 November 2017
Geosphere (2018) 14 (1): 23–49.
...., 1989 ; Trop et al., 2005 ; Trop and Ridgway, 2007 ), Chugach ( Bol and Roeske, 1993 ), and Yakutat ( Plafker et al., 1978 , 1994 ); (3) subduction of a spreading center in late Paleocene to early Eocene time (e.g., Bradley et al., 2000 ), and possibly an earlier one in the Early Cretaceous ( Pavlis...
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Series: GSA Field Guide
Published: 01 January 2008
DOI: 10.1130/2008.fld011(03)
EISBN: 9780813756110
... fault; BM—Black Mountains; BP—Big Pine; Br—Baker; Bw—Barstow; By—Beatty; CA—California; CF—Cady fault; CLF—Coyote Lake fault; CoF—Calico fault; CRF—Camp Rock fault; DSF—Deep Springs fault; DV-FLVF—Death Valley–Fish Lake Valley fault; EPF—Emigrant Peak fault; EV—Eureka Valley; FIF—Fort Irwin fault; FM...
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Journal Article
Published: 01 January 2006
Micropaleontology (2006) 52 (1): 1–50.
... (1990) proposed a Zone of Paraboultonia for the last fusulinacean interval at the top of the Guadalupian. Recently, Wilde et al. (1999) formally introduced the name Reef Trail Member for the “post-Lamar” strata at the top of the Bell Canyon Formation and illustrated fusulinaceans from four...
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Journal Article
Journal: GSA Bulletin
Published: 21 November 2019
GSA Bulletin (2020) 132 (7-8): 1537–1565.
... almost continuously for ∼7 km along California State Highway 127 to its intersection with the Old Spanish Trail ( Fig. 2 ; Hillhouse, 1987 ) and thence southeastward ∼3 km ( Olson, 2014 ). Brownish mud and sandy mud with carbonate masses constituting an ∼5–8-m-thick interval below the Tecopa tuff...
FIGURES | View All (12)
Journal Article
Journal: SEG Discovery
Published: 01 October 2013
SEG Discovery (2013) (95): 1–48.
Journal Article
Published: 01 January 1939
Bulletin of the Seismological Society of America (1939) 29 (1): 1–297.