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Satanka Formation

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Journal Article
Journal: AAPG Bulletin
Published: 01 January 1962
AAPG Bulletin (1962) 46 (1): 46–59.
... shale marker” in Cheyenne County, Nebraska. The Satanka Formation consists of the predominantly red sediments that lie between the Casper or Ingleside Formation below and the Opeche Shale or the Lyons Sandstone above. Lateral equivalents of the Satanka are the uppermost Casper of the type locality...
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Journal Article
Published: 01 October 1965
Rocky Mountain Geology (1965) 4 (2): 81–84.
...Michael D. Fenton; M. R. Voorhies Abstract Highly contorted siltstone strata of the Satanka Formation (Permian) are exposed in a stream bank northeast of Laramie, Wyo. Overlying the Satanka at this locality are Pleistocene fluviatile sediments (several lenses of sand and a bed of cobbles) which...
Image
Cross section from north to south along Front Range from Wyoming line to so...
Published: 01 August 1950
Fig. 5.— Cross section from north to south along Front Range from Wyoming line to southern Colorado showing stratigraphic relations of lower Lykins, Satanka of southern Wyoming, Lyons sandstone, Ingleside, and upper Fountain formation.
Journal Article
Journal: AAPG Bulletin
Published: 01 December 1934
AAPG Bulletin (1934) 18 (12): 1655–1697.
... of various investigators led the writer to make a detailed stratigraphic study of the relations of the Phosphoria and the Dinwoody formations to the red-bed “Embar” of central Wyoming and to the red Satanka shale, the Forelle limestone, and the Chugwater red beds of the Laramie Basin. In 1906, Darton 3...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 1949
AAPG Bulletin (1949) 33 (1): 52–72.
.... This “Lyons facies” is interstratified, above, below, and even within, with sediments whose characteristics group them naturally either with underlying or overlying formations; that is the Fountain formation; the lower Lykins formation; or the upper and lower Satanka tongues. Fountain sedimentation...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1973
AAPG Bulletin (1973) 57 (11): 2217–2244.
... the Lyons, and much of the Lyons in the east appear to contain leached anhydrite as illustrated ( Fig. 21 ). The anhydrite of the “upper Satanka” capping formation is uniformly of the normal variety, indicating that it was unaffected by solution activity. Fig. 21 —Vertical section showing anhydrite...
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Journal Article
Journal: AAPG Bulletin
Published: 01 May 1941
AAPG Bulletin (1941) 25 (5): 947–948.
... aurice M undorf , Cincinnati University, Cincinnati, Ohio Fusulinidae from Phosphoria in Montana 5. Harold B. Renfro, University of Wisconsin, Madison, Wisconsin Faunal Correlation of Satanka and Lykins Formations 6. J. H arlan J ohnson , Colorado School of Mines, Golden, Colorado...
Journal Article
Published: 01 November 2023
Rocky Mountain Geology (2023) 58 (2): 57–82.
... ; Berman, 1978 ; Sonnenberg, 1981 ; Nair et al., 2018 ) and fine-grained mudstone and sandstone of the restricted marine-to-continental-facies of the Owl Canyon Formation (formerly known as the “Satanka Formation” in northeast Colorado; Dimelow, 1972 ; Pearson, 1972 ; Courtright, 1974 ; Maughan, 1980...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1933
AAPG Bulletin (1933) 17 (2): 109–168.
... the “Crinkled limestone” at Owl Canyon are also included in the Lykins and are correlated with the Chugwater of Wyoming which is classed as Lower Triassic. The “Cross-bedded sandstone” persists to the Wyoming line and perhaps a short distance beyond, where it feathers out into the Satanka shale. This formation...
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Journal Article
Journal: AAPG Bulletin
Published: 01 June 1930
AAPG Bulletin (1930) 14 (6): 765–788.
.... Along the east side of the Front Range element, red clays, silts, and sands accumulated to form the Lykins formation. This formation also contains much gypsum, indicating an absence of land-derived sediment. In southern Wyoming, the Forelle and Satanka formations occupy the basal part of the succession...
FIGURES
Journal Article
Published: 01 September 2017
Journal of Environmental and Engineering Geophysics (2017) 22 (3): 249–266.
... of three shallow-dipping, sub-horizontal layers in the near surface: an unconsolidated clay loam, the Satanka Formation, and the Epsilon Sandstone Member of the Casper Formation. The unsaturated 3-4 m thick clay loam is a low-resistivity layer that overlies the lower-resistivity silty-claystone...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1944
AAPG Bulletin (1944) 28 (8): 1196–1216.
... Tensleep (also called Casper) formation. These beds consist of cross-bedded sandstones and interbedded sandstones and limestones. Overlying the Tensleep formation are the Permian Satanka red shales and thin limestones, about 200 feet in total thickness. The 15-foot thick Permian Forelle limestone separates...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1950
AAPG Bulletin (1950) 34 (8): 1659–1698.
...Fig. 5.— Cross section from north to south along Front Range from Wyoming line to southern Colorado showing stratigraphic relations of lower Lykins, Satanka of southern Wyoming, Lyons sandstone, Ingleside, and upper Fountain formation. ...
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Journal Article
Journal: AAPG Bulletin
Published: 01 June 1959
AAPG Bulletin (1959) 43 (6): 1370–1378.
... Company. The deepest formations reached were the Ordovician Arbuckle, the Mississippian (St. Louis?) and the Cambrian Reagan (25). Much needed stratigraphic data will come from these exploratory failures. The lower Satanka (Permian) was tested by the Brinkerhoff Drilling Company on the west side...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 December 1957
AAPG Bulletin (1957) 41 (12): 2603–2676.
... formation near Colorado Springs. Elsewhere the Fountain formation is at the base. Ingleside formation, Lyons sandstone, Satanka shale, Forelle-Glennon limestone, Lykins-Chugwater formation, Jelm-Entrada sandstones, and the Morrison formation occur in stratigraphic succession. Jelm, Ingleside, and Satanka...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1994
AAPG Bulletin (1994) 78 (2): 217–237.
... and Pennsylvanian shales ( Levandowski et al., 1973 ), (2) the Permian Satanka Formation ( Berman, 1978 ), or (3) the Permian Phosphoria Formation near the Idaho-Wyoming border ( Dimelow, 1972 ; Momper, 1978 ). The third theory seems unlikely because the oils differ in carbon isotopic composition from...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1950
AAPG Bulletin (1950) 34 (7): 1540–1551.
... of the Phosphoria formation,” Missouri Univ. Studies , Vol. 5, No. 2 (1030), pp. 1–99. 3 Phosphoria formation, Southern Absaroka Range, Wyoming: Love, J. D., “Geology along the Southern Margin of the Absaroka Range, Wyoming,” Geol. Soc. America Spec. Paper 20 (1930), p. 35. 4 Limestone in Satanka...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1966
AAPG Bulletin (1966) 50 (2): 227–250.
... across southeastern Montana. This flexure, here named the Rosebud arch, trended northeast from the northern end of the Big Horn Mountains and served as a barrier to the northward advance of the sea. On this arch the formations are markedly thin, as shown on the Lower Pennsylvanian isopachous map ( Fig. 5...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1965
AAPG Bulletin (1965) 49 (11): 1893–1907.
... contain facies changes which in other formations produce effective stratigraphic traps. Rock Unit II contains strata of Ordovician age which thin southward because of depositional onlap and Devonian-Silurian erosion. The strata of Rock Unit II contain facies changes and porosity pinch-outs in beds...
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Journal Article
Journal: AAPG Bulletin
Published: 11 December 1998
AAPG Bulletin (1998) 82 (12): 2173–2191.
... of variable thicknesses of salt encountered in the Satanka and Lyons intervals. Additionally, late Paleozoic formations in the northern Denver basin are slightly underpressured, except for several thin, nitrogen-bearing dolomite zones in the upper Council Grove and lower Chase Group that are encased...
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