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Cody Creek Formation

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Lithologies of <b>Cody</b> <b>Creek</b> <b>Formation</b>.  A.  Exposure of medium- to coarse-gra...
Published: 01 June 2013
Figure 8 Lithologies of Cody Creek Formation. A. Exposure of medium- to coarse-grained cross-stratified sandstone, Locality L on Figure 1 . B. Close-up photograph showing details of cross-stratification, Locality L. C. Plant megafossils preserved in cross-stratified sandstone, Locality K
Journal Article
Published: 01 June 2013
Bulletin of Canadian Petroleum Geology (2013) 61 (2): 101-132.
...Figure 8 Lithologies of Cody Creek Formation. A. Exposure of medium- to coarse-grained cross-stratified sandstone, Locality L on Figure 1 . B. Close-up photograph showing details of cross-stratification, Locality L. C. Plant megafossils preserved in cross-stratified sandstone, Locality K...
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Series: AAPG Memoir
Published: 01 January 1986
DOI: 10.1306/M41456C22
EISBN: 9781629811451
... in the lowermost Cody Formation. These variations in thickness in the lower Cody may have started late during the time of Wall Creek sandstone deposition, and they may be related to deposition of the uppermost sandstones of the Wall Creek, which produce hydrocarbons from stratigraphic traps in the deep part...
Image
Detrital zircon populations, sample 77EAB07, collected from <b>Cody</b> <b>Creek</b> Form...
Published: 01 June 2013
Figure 13 Detrital zircon populations, sample 77EAB07, collected from Cody Creek Formation at UTM 377650E, 7304923N (NAD27) ( Fig. 1 , Locality X). A. Total zircon population. B. Younger fraction.
Series: SEPM Special Publication
Published: 01 January 1984
DOI: 10.2110/pec.84.34.0085
EISBN: 9781565761643
... abstract Two vertically stacked shelf-ridge (bar) complexes in the Shannon Sandstone member of the Cody Shale (designated upper and lower sandstones) crop out in the Salt Creek anticline of the Powder River Basin, Wyoming. The shelf-ridge complexes are composed primarily of moderately to highly...
Image
Left:   Stratigraphic section of sandy member of <b>Cody</b> Shale at Sheep <b>Creek</b> ...
Published: 01 January 2007
Figure 3. Left: Stratigraphic section of sandy member of Cody Shale at Sheep Creek in T. 6 N, R. 2 E, Fremont County, Wyoming. Modified from Keefer and Troyer (1956 ; 1964 : 87–89, pl. 2). Right: Stratigraphic section of upper part of Kevin Member of Marias River Shale, Telegraph Creek
Series: SEPM Special Publication
Published: 01 January 1964
DOI: 10.2110/pec.64.01.0153
EISBN: 9781565761414
... Abstract The Upper Cretaceous Frontier Formation in northwestern Wyoming consists of alternating sandstone and shale, interbedded with coal, lignite, bentonite and tuff. The formation varies in thickness from about 600 feet to more than 2000 feet. At Little Horse Creek, in the northwestern end...
Journal Article
Journal: AAPG Bulletin
Published: 01 February 2000
AAPG Bulletin (2000) 84 (2): 210-233.
...Daniel J. Miller; Kenneth A. Eriksson Abstract The Upper Mississippian Hinton, Princeton, and Bluestone formations of southern West Virginia constitute a westward-thinning wedge of strata that filled the central Appalachian basin over approximately 7 m.y. Up to 17 transgressive-regressive sequences...
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Journal Article
Journal: AAPG Bulletin
Published: 01 April 2017
AAPG Bulletin (2017) 101 (4): 419-421.
... such cycles. REFERENCE CITED Feldman H. R. Fabijanic J. M. Faulkner B. L. Rudolph K. T. , 2014 , Lithofacies, parasequence stacking, and depositional architecture of wave- to tide-dominated shorelines in the Frontier Formation, western Wyoming, U.S.A : Journal of Sedimentary...
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Outcrop photographs of Burnthill <b>Creek</b> <b>Formation</b>.  A.  Exposures of lower p...
Published: 01 June 2013
-clastic sedimentation preceding the onset of Cody Creek Formation deposition.
Journal Article
Journal: Elements
Published: 01 June 2005
Elements (2005) 1 (3): 139-143.
... and Wächtershäuser 1997 ), suggests another route to the formation of key metabolic molecules, such as pyruvic acid and other so-called “alpha ketoacids”. Thus, Cody et al. ( 2000 ) explored whether, under high pressure, reactions of alkane thiols, carbon monoxide, and FeS might provide a source of alpha ketoacids...
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Series: SEPM Short Course Notes
Published: 01 January 2007
DOI: 10.2110/pec.07.52.0343
EISBN: 9781565761407
... rare (vr), rare (r), moderate (m), common (c), and abundant (a). The Turonian Wall Creek Member of the Frontier Formation, along with similar shore- parallel isolated Cretaceous sandbodies encased in shelf-mud of the Cretaceous Interior Seaway of North America, has traditionally been interpreted...
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Journal Article
Published: 27 August 2008
Canadian Journal of Earth Sciences (2008) 45 (7): 827-859.
...Michael C. Wilson; Leonard V. Hills; Beth Shapiro Abstract Late Pleistocene bison skeletal remains from the Gallelli Gravel Pit in the Bighill Creek Formation at Calgary, Alberta, document at least two individuals, including the largest postglacial bison reported from North America south...
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Journal Article
Journal: Geosphere
Published: 01 June 2017
Geosphere (2017) 13 (3): 950-973.
...Glenn R. Sharman; Theresa M. Schwartz; Lauren E. Shumaker; Cody R. Trigg; Nora M. Nieminski; Zachary T. Sickmann; Matthew A. Malkowski; Jeremy K. Hourigan; Benjamin J. Schulein; Stephan A. Graham Abstract Outcrops within the Eocene Domengine Formation (central California) provide an exceptional...
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Journal Article
Journal: AAPG Bulletin
Published: 01 December 1939
AAPG Bulletin (1939) 23 (12): 1751-1819.
... of Oklahoma, while the selenite-veined Flower-pot shales, 190 feet thick, have been called Chickasha in Oklahoma. The name “Nippewalla” is suggested for the group of formations lying between the Stone Corral and Blaine evaporites. Cragin’s “Cave Creek formation” is identical with the Blaine formation...
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Series: GSA Field Guide
Published: 01 January 2016
DOI: 10.1130/2016.0041(06)
EISBN: 9780813756417
... and 5 ; Kauffman et al., 2014 ). Subsequent Permian to Late Trias-sic arc magmatism and sedimentation are recorded by the Seven Devils Group ( Vallier, 1977 ). The Seven Devils Group includes felsic and mafic volcanogenic rocks of the Permian Windy Ridge and Hunsaker Creek Formations, overlying...
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Journal Article
Published: 01 January 2012
Rocky Mountain Geology (2012) 47 (1): 55-79.
... ). Transport along the SFFS emplaced Jurassic through Eocene rocks onto a possible bedding-plane detachment within the Cretaceous Cody Shale and cut upward through the Eocene Willwood Formation. The area west of the Hardpan Tear Fault shows a simple, ramp geometry (cross section D–D′; Fig. 3 ), placing...
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Journal Article
Journal: AAPG Bulletin
Published: 01 June 2000
AAPG Bulletin (2000) 84 (6): 830-849.
... nose of the anticline. The contact of the Frontier and Cody formations is faulted in the southern and southwestern portions of the anticline. Near cross section C and between cross sections C and D ( Figure 4a ), there are two tear faults, each with approximately 10 m of apparent right-lateral...
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Journal Article
Journal: Economic Geology
Published: 01 November 2009
Economic Geology (2009) 104 (7): 945-960.
... and related compressional terranes provide a fundamentally important role in the formation of those mesothermal-style vein deposits. At Rock Creek late-and postore transpressional fabrics superimposed on the extensive mesh of tension veins show similarly that transpression played a key role in the evolution...
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Series: AAPG Studies in Geology
Published: 01 January 2013
DOI: 10.1306/13381689St653578
EISBN: 9781629812632
..., the Parkman Sandstone Member of the Mesaverde Formation, the Shannon Sandstone bed of the Steele Member of the Cody Shale, and the Frontier Formation. Lacking downhole temperature data, Naeser (1992) calculated present-day sample temperatures using a mean geothermal gradient from geothermal gradient maps...
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