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Title: Model for sandstone-carbonate cyclothems based on upper member of Morgan Formation (Middle Pennsylvanian) of Northern Utah and Colorado

Journal Article · · Am. Assoc. Pet. Geol., Bull.; (United States)
OSTI ID:5504626

The upper member of the 200 m (660 ft) thick Morgan Formation (Middle Pennsylvanian) consists of 5-25 m (16-82 ft) thick, very fine-grained quartz sandstone units that are interbedded repetitively with 0.5-11 m (1.6-36 ft) thick, oolitic, bioclastic, peloidal, and micritic carbonate units. Similar repetitive sequences occur widely in western North America. The quartz sandstone-carbonate cyclothems defined by this study have potential as targets for hydrocarbon exploration. Both eolian dune sandstones and dolomitized shelf carbonate strata are locally important reservoir rocks in the subsurface in parts of the western Overthrust belt in Utah and Wyoming. 84 references, 22 figures, 4 tables.

Research Organization:
Univ. of Wisconsin, Madison
OSTI ID:
5504626
Journal Information:
Am. Assoc. Pet. Geol., Bull.; (United States), Vol. 68:5
Country of Publication:
United States
Language:
English