Upper Fort Union coals in western Powder River Basin, Wyoming: alluvial-plain deposits

Conference · Sun Apr 01 04:00:00 EST 1984 · Am. Assoc. Pet. Geol., Bull.; (United States)

OSTI ID:6561358

Flores, R M; Hardie, J K; Coss, J M; Weaver, J N; Van Gosen, B S

Stratigraphic distribution of coals and associated lithofacies in the upper Fort Union Formation (Paleocene) was investigated in outcrop and subsurface from southeast of Sussex to south of Buffalo, Wyoming. In this area, Ayers and Kaiser in 1982 proposed that upper Fort Union coals accumulated in deltas and interdeltas, and pinched out into a lake. Our study does not support these interpretations. The upper 1000 ft (300 m) of the Fort Union Formation in the western Powder River basin comprises interbedded conglomerates, conglomeratic sandstones, sandstones, siltstones, mudstones, carbonaceous shales, and coals. The conglomerates, consisting of pebbles and cobbles reworked from Mesozoic and Paleozoic rocks, are in scour-based bodies as thick as 25 ft (8 m). A 300-ft (90 m) thick, 12-mi (19 km) long conglomeratic channel-sandstone complex is in the lower part of the interval. In the upper part of the interval, conglomeratic single- and multistory channel sandstones reach thickness of 100 ft (30 m) and widths of 4000 ft (1200 m). These channel sandstones grade into overbank-floodplain sediments, which are interbedded with backswamp deposits of coals and carbonaceous shales. The conglomeratic channel sandstones are interbedded with coal beds as thick as 20 ft (6 m). These coal beds probably are laterally equivalent to the 178-ft (54 m) thick Sussex coal deposit to the east. Lithofacies associated with the coals in the western Powder River basin suggest an alluvial-plain paleoenvironment. The alluvial plain consisted of braided and meandering streams flanked by well-drained and poorly drained backswamps. These streams probably are northeasterly flowing tributaries of trunk streams.

• Research Organization: Geological Survey, Denver, CO
• OSTI ID: 6561358
• Report Number(s): CONF-8405216-
• Conference Information: Journal Name: Am. Assoc. Pet. Geol., Bull.; (United States) Journal Volume: 68:4
• Country of Publication: United States
• Language: English

Related Subjects

01 COAL, LIGNITE, AND PEAT
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BITUMINOUS MATERIALS
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CENOZOIC ERA
CHATTANOOGA FORMATION
COAL DEPOSITS
DEPOSITION
ENERGY SOURCES
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SEDIMENTARY BASINS
SEDIMENTARY ROCKS
STRATIGRAPHY
TERTIARY PERIOD
USA
WYOMING