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1-4 OF 4 RESULTS FOR
Parkman Sandstone
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Series: AAPG Studies in Geology
Publisher: American Association of Petroleum Geologists
Published: 01 January 2013
DOI: 10.1306/13381693St653571
EISBN: 9781629812632
Abstract In sedimetary basins not currently undergoing primary compaction (e.g., Rocky Mountain Basins), p-wave velocities noticeably vary with azimuth, yet the mechanism(s) controlling the anisotropy remain uncertain. Possible geologic causes for azimuthal anisotropy include but are not limited to sedimentary fabrics, steep bedding, changes in local in-situ or residual stress, and open or mineralized fractures. To test these hypotheses, P-wave velocity azimuths (Vfast) from a proprietary seismic survey of a NNW-trending Laramide Anticline on Casper Arch in central Wyoming were compared to image log data from the seismic coverage area and fracture orientations from nearby analog structures.
Journal Article
Comment regarding Piney Creek thrust fault, Sheridan County, Wyoming
Journal: Rocky Mountain Geology
Publisher: University of Wyoming
Published: 01 April 1986
Rocky Mountain Geology (1986) 24 (1): 103.
Journal Article
Discovery of Upper Cretaceous “Parkman Sandstone” Production, Denver Basin, Colorado
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 May 1985
AAPG Bulletin (1985) 69 (5): 850.
Journal Article
Sedimentology of Upper Cretaceous Cody-Parkman Delta, Southwestern Powder River Basin, Wyoming
Journal: GSA Bulletin
Publisher: Geological Society of America
Published: 01 June 1972
GSA Bulletin (1972) 83 (6): 1649–1670.
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Parkman Sandstone
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