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Geology and petrology of Tertiary lignites adjacent to Beartooth Mountain Front, Montana-Wyoming

Conference · · Am. Assoc. Pet. Geol., Bull.; (United States)
OSTI ID:6562779
Along the eastern margin of the Beartooth front a sequence of Laramide conglomerates, sandstones, siltstones, shales, and minor coals are exposed. These minor Paleocene-Eocene coals, ranging from lignite to subbituminous in rank, are the focus of this study. Four coal exposures were sampled along a north-south strip (17 mi, 27 km), proximal to the Beartooth front. These coals range in thickness from less than a 1-in. (2.5 cm) lens to about 10 ft (3 m) and contain partings of carbonaceous shale, shale, siltstone and sandstone. Two of the seams, designated as Meeteetse trail and Burgess Lignite occur in typical Fort Union sediments. The other, the Burgess Lignite locality, is composed of alternating papery fusinitic lignite, siltstones, thin lenses of channel sandstones, carbonaceous shales, and carbonaceous mudstones. The coals here are high in organic matter, fossil stems, leaves, megascopic resins, randomly oriented petrified tree stumps, and gypsiferous deposits. Two other localities, Gold Creed and Clarks Fork Canyon, are in Paleocene alluvial fan deposits. The Clarks Fork coals are found at the distal end of an alluvial fan system and dip rather gently basinward. The Gold Creek coals are found at the base of a fan interbedded with massive sandstones and conglomerates containing andesitic porphyry clasts up to 1.5 ft (0.4 m) in maximum dimension. The Fort Union Formation in this area includes lacustrine, paludal, fluvial, and conglomeratic members. Petrographic examination reveals well preserved cell structure, especially in the fusinoid macerals. Although the coals have undergone severe alteration and weathering, they still exhibit excellent fluorescence properties.
Research Organization:
Southern Illinois Univ., Carbondale
OSTI ID:
6562779
Report Number(s):
CONF-8310301-
Conference Information:
Journal Name: Am. Assoc. Pet. Geol., Bull.; (United States) Journal Volume: 67:9
Country of Publication:
United States
Language:
English