Stratigraphic Entrapment of Cretaceous Hydrocarbons, Green River Basin, Wyoming

Stratigraphic Entrapment of Hydrocarbons in the Upper Cretaceous Lewis Shale and Lower Fox Hills Sandstone, Eastern Green River Basin, Wyoming
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A presentation to the HGS North American Explorationists Group, April 26, 2004
 
D.S. Muller and F.T Wirnkar, BP America, <?xml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />501 Westlake Park Blvd., Houston TX  77079
 
Abstract: The Eastern Green River Basin is an active hydrocarbon province in central Wyoming.  BP America is involved in a multi-rig, multi-year program and currently has seven rigs operating.  Production is primarily from tight Cretaceous sandstones requiring hydraulic fracture stimulation to produce at economic rates.
 
Early exploration and development in the eastern Green River Basin was primarily driven by high production rates associated with shoreline deposits at the top of the Almond Fm,.  These sands and underlying paralic and coastal plain deposits of the Almond were deposited during the final transgression of the Cretaceous cratonic seaway of  the central United States.  Much of the subsequent development in the basin has targeted less extensive sands deposited within the Main Almond in the environments behind the transgressive/stillstand bar deposits.
 
The Almond Fm is overlain by the Lewis Shale.  The Asquith Marker, a regionally recognizable Maximum Flooding Surface within the lower Lewis, marks the overall transition from the transgressive phase to the regressive episode associated with the infilling.  Above the Asquith marker, the overlying sediments of the remainder of the Lewis and overlying Fox Hills and Lance Fms accomplished the final in-filling of this last phase of the Cretaceous intracratonic seaway.
 
Hydrocarbons within the regressive phase of this third order filling cycle have increasingly been recognized and targeted as drilling has progressed in the basin.  This presentation addresses the stratigraphy, trapping configuration, results, and recent developments associated with the younger strata of the Lewis Shale and Fox Hills Sandstone in the eastern Green River Basin.  Stratigraphic traps within the Upper Cretaceous Lewis and Fox Hills of the Red Desert Basin occur in sands deposited within basin floor fans, slope fans, lowstand wedge deposits, shelf margin deltas, and in nearshore marine environments associated with the final major regression of the Western Interior Cretaceous Seaway.  Lewis gas and condensate are generally produced as part of a co-mingled production stream together with gas from the underlying Almond Fm. of the Mesaverde Group.  Production logs and standalone Lewis producers demonstrate that the Lewis is locally a very significant component of the hydrocarbon production stream within the Red Desert Basin portion of the Eastern Green River Basin
 
Entrapment in Lewis Shale within the Red Desert Basin occurs at the now updip, distal edges of sand packages that were deposited from a northerly provenance (“Red Desert Delta” or “Sheridan Delta”) within and near the margins of the Lewis seaway during the Maastrichtian.  Geometries, log character, seismic data, and other characteristics of the sands within the Lewis shale for a number of different traps at several stratigraphic levels indicate that deposition occurred in a variety of settings.
 
Speaker Biography: Dave Muller received his Bachelor’s degree in Geology from Colgate University in 1977.  He wa