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Cathedral Bluffs Member

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Journal Article
Published: 01 June 2010
Journal of Sedimentary Research (2010) 80 (6): 492–514.
... Ma. Prior to this transition, drainage entered the basin from the east and the arkosic detritus of the Cathedral Bluffs Member of the Wasatch Formation was deposited in the Washakie and Great Divide subbasins. At the same time evaporitic sediments of the Wilkins Peak Member of the Green River...
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Journal Article
Published: 01 July 2001
Journal of Paleontology (2001) 75 (4): 901–904.
... and worked by P. O. McGrew and is University of Wyoming locality V-58006. The quarry is approximately 30 m below the top of the Cathedral Bluffs Tongue ( McGrew, 1980 ), which is between the lacustrine Tipton Shale and Laney members of the Green River Formation. Fossils from the Cathedral Bluffs Tongue...
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Journal Article
Published: 01 November 2012
Journal of Paleontology (2012) 86 (6): 973–978.
... smaller than Uintasorex montezumicus from California. Both the newly described taxon and U. montezumicus are among the smallest plesiadapiforms yet known with body weights estimated to be 20 to 25 g. The sediments of the Cathedral Bluffs Tongue of the Wasatch Formation at South Pass contain a unique...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1968
AAPG Bulletin (1968) 52 (11): 2249–2256.
... in measured sections to a 188- to 325-ft-thick sequence of mainly brown, platy to papery,low-grade oil shale 4 beneath the “beds representing Laney shale member and Cathedral Bluffs red beds member” (the unit subsequently renamed the Wilkins Peak Member by Bradley, 1959 ). Southeast of the Rock Springs...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1985
AAPG Bulletin (1985) 69 (6): 913–922.
... by Oriel (1961) in outcrops along the western margin of the basin; (2) nine arkosic sandstone-siltstone marker units interbedded in the Wilkins Peak Member identified by Culbertson (1961) in the southeastern region; and (3) Cathedral Bluffs Tongue in the Washakie basin. The only fluvial clastic unit...
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Journal Article
Published: 01 November 2006
Journal of Sedimentary Research (2006) 76 (11): 1197–1214.
... members and grades laterally into variegated red and green alluvial mudstone and sandstone of the Cathedral Bluffs Tongue of the Wasatch Formation ( Fig. 2 ). On the basis of recent 40 Ar/ 39 Ar geochronology, the Wilkins Peak Member spans approximately 1 My ( Smith et al. 2003 ). The Wilkins Peak Member...
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Journal Article
Journal: GSA Bulletin
Published: 01 January 2010
GSA Bulletin (2010) 122 (1-2): 236–252.
...Amalia C. Doebbert; Alan R. Carroll; Andreas Mulch; Lauren M. Chetel; C. Page Chamberlain Abstract Oxygen isotope values from lacustrine carbonate in the Laney Member of the Green River Formation (Wyoming) exhibit a sudden, basinwide, ∼6‰ upsection decrease in δ 18 O at ca. 49 Ma. 40 Ar/ 39 Ar...
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Series: GSA Field Forum Field Trip Guides
Published: 01 January 2005
DOI: 10.1130/2005.IAAEOM.FFG-p3
EISBN: 9780813759371
...), the granodiorite of Kuna Crest and the tonalite of Glen Aulin (93.5-93.1 Ma; assumed to represent the eastern and western parts of the same intrusion; Bateman and Chappell, 1979), the Half Dome Granodiorite (92.8-88.8 Ma), the Cathedral Peak Granodiorite (88.1-86 Ma), and the Johnson Granite Porphyry (85 Ma; Fig...
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Image
High-resolution stratigraphic cross section of the Wilkins Peak <b>Member</b> at W...
Published: 01 November 2006
Figure 11 High-resolution stratigraphic cross section of the Wilkins Peak Member at White Mountain. See Figure 1 for location of measured sections. Letters A–I correspond to the nine units of the fluvial association ( Culbertson 1961 ). CBT, Cathedral Bluffs Tongue. Detailed versions of all
Image
Generalized Laney <b>Member</b> stratigraphy, with representative lithology, δ 18 ...
Published: 01 January 2010
Figure 2. Generalized Laney Member stratigraphy, with representative lithology, δ 18 O, and 87 Sr/ 86 Sr from the Washakie Basin #1 core (WB1). Units represented include the Cathedral Bluffs Tongue of the Wasatch Formation (CB), the Wilkins Peak Member of the Green River Formation (WP
Series: AAPG Memoir, AAPG Memoir
Published: 01 January 2012
DOI: 10.1306/13291391M953451
EISBN: 9781629810096
... Formation. NLT = Niland Tongue of the Wasatch Formation. CBT = Cathedral Bluffs Tongue of the Wasatch Formation. Calcite (CaCO 3 — hexagonal) was identified almost continuously throughout the Laney and Tipton members of the Green River Formation. Calcite decreased in abundance at the top...
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Journal Article
Journal: GSA Bulletin
Published: 01 May 2003
GSA Bulletin (2003) 115 (5): 549–565.
... al. (1997) presented magnetostratigraphy of a section on the western edge of the Greater Green River Basin encompassing the main body of the Wasatch Formation, the Tipton and Wilkins Peak Members, the Cathedral Bluffs Tongue, and the Laney Member ( Roehler, 1989 ). Clyde et al. (2001) added...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2009
DOI: 10.1144/SP317.20
EISBN: 9781862395657
... Abstract From its earliest years the Geological Society of London attracted the attention of scientifically- and technically-minded men in Australia and New Zealand. Members ‘at home’ in Britain were also eager for geological information about the antipodes. The publications of the Society...
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Journal Article
Journal: AAPG Bulletin
Published: 01 March 1954
AAPG Bulletin (1954) 38 (3): 405–425.
...Carle H. Dane ABSTRACT The Parachute Creek member of the Green River formation is an approximately time-equivalent zone across the Uinta Basin of Utah, as shown by the correlation of extensive thin tuff beds within the member. The top of the overlying Evacuation Creek member is regarded as the base...
FIGURES
Journal Article
Journal: GSA Bulletin
Published: 01 January 2008
GSA Bulletin (2008) 120 (1-2): 54–84.
... al., 2003a ), and is laterally equivalent to alluvial deposits of the Cathedral Bluffs Member of the Wasatch Formation in adjacent subbasins ( Sullivan, 1985 ; Roehler, 1992a ). The fluctuating profundal to fluviallacustrine LaClede bed of the Laney Member overlies the Wilkins Peak Member...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1938
AAPG Bulletin (1938) 22 (8): 1020–1047.
... tongue of the Green River formation and the highest productive petroleum horizon in the Hiawatha member. No indications of petroleum are known to occur in the Cathedral Bluffs member or the upper several hundred feet of the Hiawatha member. Immediately underlying the Hiawatha member of the Wasatch...
FIGURES
Journal Article
Published: 01 April 2017
Journal of Sedimentary Research (2017) 87 (4): 406–423.
... strata in the Bridger Basin from time-equivalent alluvial deposits of the Cathedral Bluffs Member of the Wasatch Formation to the east ( Figs. 1 , 2 ; Sullivan 1985 ; Roehler 1993 ; Smith et al. 2008 ; Chetel et al. 2011 ). The Rock Springs Arch appears to have acted as a partial topographic barrier...
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Journal Article
Journal: GSA Bulletin
Published: 01 January 2000
GSA Bulletin (2000) 112 (1): 119–135.
...-member models (e.g., fracture vs. diapir) are oversimplifications of the pluton assembly process. Figure 5. Map of magmatic foliations as measured in the field. Figure 1. Map of the Mount Givens pluton showing compositional and textural facies and U-Pb localities (after Bateman, 1992...
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Image
Stratigraphic diagram for the southern Greater Green River Basin. Modified ...
Published: 01 January 2009
. (2006) . The Niland and Cathedral Bluffs Tongues are members of the Wasatch Formation that inter-finger with the Luman, Tipton Shale, Wilkins Peak, and Laney members of the Green River Formation. North American Land Mammal Age (NALMA) abbreviations: To 2 , Torrejonian Subage 2; To 3 Torrejonian Subage
Image
Figure 2. Stratigraphic framework for the seven floral assemblages (filled ...
Published: 01 February 2000
Formation (fluvial); Tw—Wasatch Formation (fluvial): Twm—Main Body, events interpolated using Roehler (1992c) and Hutchison (1980) ; Twrr—Ramsey Ranch Member; Twn—Niland Tongue; Twc—Cathedral Bluffs Tongue. Tg—Green River Formation (lacustrine): Tglu—Luman Tongue; Tgt—Tipton Shale Member; Tgw—Wilkins