1-15 OF 15 RESULTS FOR

cathedral bluffs-laney beds contact

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article
Published: 01 June 2010
Journal of Sedimentary Research (2010) 80 (6): 492–514.
... and Laney members may correlate to an unconstrained position at or near the top of the Cathedral Bluffs Member in the Washakie Basin ( Fig. 16A ). The base of the I-bed, the uppermost arkosic marker bed of the Wilkins Peak Member, in the Bridger Basin correlates with an unknown position in the Washakie...
FIGURES | View All (17)
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...
FIGURES | View All (9)
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1930
AAPG Bulletin (1930) 14 (8): 1013–1040.
... somewhat younger than Wasatch. Farther out, on the east and southeast, Cathedral Bluff red beds of upper Wasatch age rise to form the Kinney Rim escarpment ( Fig. 2 ). In the southwest part of the mapped area, rocks ranging in age from Cretaceous to Cambrian occur between the Sparks fault and Cold Spring...
FIGURES | View All (5)
Journal Article
Journal: GSA Bulletin
Published: 01 January 2010
GSA Bulletin (2010) 122 (1-2): 236–252.
... the idea of nearby high relief. The lower LaClede Bed of the Laney Member, originally described by Roehler (1973) , is characterized by alternation between shallow and deeper-water lithologies ( Fig. 2 ). Flooding surfaces, sometimes marked by rip-up horizons, are overlain by shallow stromatolite...
FIGURES | View All (9)
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 August 1938
AAPG Bulletin (1938) 22 (8): 1020–1047.
..., approximately 5,300 feet below the Laney shale-Cathedral Bluffs contact, and in a second well at 3,350 feet below that contact. Thus the stratigraphic interval between the two petroleum-producing horizons is 1,950 feet. A considerable interval also is present between the two gas-producing sands for the two...
FIGURES
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...
FIGURES | View All (18)
Journal Article
Journal: Geology
Published: 01 August 2015
Geology (2015) 43 (8): 691–694.
... and interfingers with the Wasatch Formation’s Cathedral Bluffs Tongue, which consists of floodplain deposits ( Roehler, 1993 ). The Green River Formation here is composed of the basal Luman Tongue, followed upsection by the Tipton Member and the Laney Member (LaClede Bed) ( Roehler, 1992 ). The depositional axis...
FIGURES
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...
FIGURES | View All (15)
Series: GSA Field Guide
Published: 01 January 2011
DOI: 10.1130/2011.0021(06)
EISBN: 9780813756219
... that the climate of the basin floor during deposition of the Niland Tongue was subtropical, without freezing temperatures. The earliest middle Eocene climates pertaining to the Cathedral Bluffs Tongue of the Wasatch Formation and the Wilkins Peak Member of the Green River Formation were interpreted as generally...
FIGURES | View All (15)
Journal Article
Published: 01 January 2009
Rocky Mountain Geology (2009) 44 (1): 1–16.
... ). We have placed the age of the upper boundary of the intermediate stratigraphic interval at approximately 52.4 Ma. The upper stratigraphic interval ( Fig. 7 ) extends from the upper contact of the Luman Tongue to the base of the Laney Member of the Green River Formation. The intervening...
FIGURES | View All (7)
Journal Article
Journal: AAPG Bulletin
Published: 01 November 1982
AAPG Bulletin (1982) 66 (11): 2509–2525.
... enabling legislation is being evaluated. Any commercialization will, of course, depend on institutional, economic, and environmental favorability. C-b (Cathedral Bluffs Shale Oil Co.) .–Cathedral Bluffs Shale Oil Co. is an equal interest partnership between Occidental Oil Shale, Inc., and Tenneco...
FIGURES | View All (9)
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...
FIGURES | View All (14)
Journal Article
Journal: GSA Bulletin
Published: 01 May 2012
GSA Bulletin (2012) 124 (5-6): 870–885.
... , 2008a) sampled the coarsest fraction of each deposit (i.e., base) in order to collect the largest possible crystals for radioisotopic dating. In one case (Boar tuff), the tuff bed was too friable for paleomagnetic sampling, so samples were collected from a siliciclastic layer immediately (∼20 cm) above...
FIGURES | View All (9)
Journal Article
Journal: GSA Bulletin
Published: 01 January 2011
GSA Bulletin (2011) 123 (1-2): 71–88.
... L.H. Stanley K.O. , 1977 , Origin of variegated red beds in the Cathedral Bluffs Tongue of the Wasatch Formation (Eocene), Wyoming : Journal of Sedimentary Petrology , v. 47 , p. 1201 – 1219 . Carroll A.R. Bohacs K.M. , 1999 , Stratigraphic classification of ancient lakes...
FIGURES | View All (9)