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GEOREF RECORD

Mississippian Madison group stratigraphy and sedimentation in Wyoming and southern Montana

John Michael Andrichuk
Mississippian Madison group stratigraphy and sedimentation in Wyoming and southern Montana
Bulletin of the American Association of Petroleum Geologists (November 1955) 39 (11): 2170-2210

Abstract

Madison sediments accumulated in 2 depositional realms - a basinal, predominantly limestone province in Montana and adjoining Dakotas; and the Wyoming shelf, characterized by prominent dolomitization on the S. The belt of transition in southern Montana and adjoining South Dakota showed relatively little migration throughout deposition. W of the Wyoming shelf, limestone and shale deposition took place in the Idaho geosynclinal trend. Southeastward to the Cambridge arch, Madison sediments were affected by increasing amounts of pre-Pennsylvanian erosion in Wyoming and western South Dakota. Mississippian sediments are absent from a part of southeastern Wyoming. Early, medial, and late stages of sedimentation may be differentiated on the basis of lithologic cycles or sequences developed in the Madison group. Early sedimentation was characterized by deposition of the approximate Lodgepole formation and equivalents, Guernsey, Englewood, and lower Pahasapa formations. Deposition commenced earliest in the Williston basin and central Montana trough with the development of black shales, followed by dense limestone and shales; minor terrestrial to nearshore marine clastic sedimentation in the Black Hills area commenced somewhat later, preceding and accompanying the initial marine transgression on the Wyoming shelf. Widespread deposition of normal marine and fragmental ooelitic limestones (mainly dolomitized equivalents in the shelf areas) occurred. Shoaling was prominent, and as a result local minor restricted deposition took place. Marine limestone and dolomite sedimentation, modified by 2 episodes of evaporite precipitation, occurred during medial Madison time. Mission Canyon carbonates containing an intermediate evaporite zone and overlain by the prominent basal Charles evaporites constitute the resulting middle unit. Evaporitic deposition was characterized by the precipitation of anhydrite and halite in the basinal areas at the N. Southward, progressively less restriction is demonstrated by the disappearance of halite, thinning of anhydrite, and the development of primary dense carbonate zones. Late sedimentation was characterized by restoration of normal marine conditions and development of a complex evaporite cycle (Charles formation, excluding basal evaporites). Big Snowy clastics were deposited in Chester time in the northern basinal areas. In other areas, pre-Amsden or pre-Pennsylvanian to pre-Middle Jurassic erosion had varying effects on the Madison surface. Limestone reservoirs in the basinal areas of Montana and North Dakota, and dolomites in northwestern Wyoming yield Madison oil. Optimum facies changes and postdepositional tectonic effects make the Madison group an excellent prospective unit in many areas.


ISSN: 0883-9247
Serial Title: Bulletin of the American Association of Petroleum Geologists
Serial Volume: 39
Serial Issue: 11
Title: Mississippian Madison group stratigraphy and sedimentation in Wyoming and southern Montana
Pages: 2170-2210
Published: 195511
Text Language: English
Publisher: American Association of Petroleum Geologists, Tulsa, OK, United States
Accession Number: 1959-041516
Categories: Areal geology
Document Type: Serial
Bibliographic Level: Analytic
N44°30'00" - N49°00'00", W116°01'60" - W104°01'60"
N41°00'00" - N45°00'00", W111°04'60" - W104°04'60"
Source Note: revised, in Goodman, A. J., ed., Jurassic and Carboniferous of western Canada, Am. Assoc. Petroleum Geologists, John Andrew Allan Memorial Volume, p. 407-449, illus., May 1958; in Weeks, L. G., ed., Habitat of oil--a symposium, p. 225-267, illus., June 1958.
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute. Reference includes data from Bibliography and Index of North American Geology, U. S. Geological Survey, Reston, VA, United States
Update Code: 1959
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