2008
DOI: 10.3133/sim3053
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Geologic map of upper cretaceous and tertiary strata and coal stratigraphy of the Paleocene Fort Union Formation, Rawlins-Little Snake River area, south-central Wyoming

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Cited by 8 publications
(14 citation statements)
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“…1) which separates it from the Washakie Basin (Love 1961;Kirschbaum et al 1994). The Granite Mountains Uplift bounds the GDB to the north, and to the east is the Rawlins Uplift which separates the GDB from the Hanna Basin (Lillegraven et al 2004;Hettinger et al 2008). During the earliest Paleocene, however, the GDB was contiguous with the Hanna Basin, and both formed part of the Greater Green River Basin (Lillegraven et al 2004;Lillegraven 2015).…”
Section: Geological Settingmentioning
confidence: 99%
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“…1) which separates it from the Washakie Basin (Love 1961;Kirschbaum et al 1994). The Granite Mountains Uplift bounds the GDB to the north, and to the east is the Rawlins Uplift which separates the GDB from the Hanna Basin (Lillegraven et al 2004;Hettinger et al 2008). During the earliest Paleocene, however, the GDB was contiguous with the Hanna Basin, and both formed part of the Greater Green River Basin (Lillegraven et al 2004;Lillegraven 2015).…”
Section: Geological Settingmentioning
confidence: 99%
“…The stratigraphy and sedimentology of the Paleocene Fort Union Formation in the GDB have been characterized in a number of studies (Hettinger et al , 2008Hettinger & Kirschbaum 1991;Honey & Hettinger 2004;Hettinger & Honey 2006). In the eastern Washakie Basin and south-eastern GDB, the Fort Union Formation is subdivided into three members that were named and described by Honey & Hettinger (2004) and Hettinger & Honey (2006): the oldest and most basal China Butte Member, the poorly exposed Blue Gap Member and the uppermost Overland Member.…”
Section: Geological Settingmentioning
confidence: 99%
“…UCM loc. 2011035 lies~50 m (166 ft) above the base of the Fort Union Formation in the China Butte Member (Hettinger et al, 2008) in the GDB. Using the North American Land Mammal Ages (NALMA) as the biochronological framework, the fauna is hypothesized to represent the early Puercan Interval Zone (Pu1).…”
Section: Geologic Settingmentioning
confidence: 99%
“…Ridge low and lingual on p4No paraconid or metaconid on p4 Distinct, lingual paraconulid (circled) Closely appressed trigonid cusps Anteriorly pitched Earliest Paleocene (Puercan) Periptychid 'Condylarths' from the Great Divide Basin, WY Atteberry, Madelaine R., University of Colorado, Boulder, CO; Eberle, Jaelyn J., University of Colorado, Boulder, CO Map of the Greater Green River Basin showing the Great Divide Basin study locality, indicated by star (modified fromHettinger et al 2008).…”
mentioning
confidence: 99%
“…Stratigraphic section showing the position of UCM locality 2011035 (modified fromHettinger et al 2008).…”
mentioning
confidence: 99%