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Structural and tectonic evolution of the Douglas Creek Arch, the Douglas Creek fault zone, and environs, northwestern Colorado and northeastern Utah; implications for petroleum accumulation in the Piceance and Uinta Basins

Jeffrey W. Bader
Structural and tectonic evolution of the Douglas Creek Arch, the Douglas Creek fault zone, and environs, northwestern Colorado and northeastern Utah; implications for petroleum accumulation in the Piceance and Uinta Basins
Rocky Mountain Geology (November 2009) 44 (2): 121-145

Abstract

The Douglas Creek arch is a north-south-trending faulted anticline that separates the Uinta basin of northeastern Utah from the Piceance basin of northwestern Colorado. Previous work indicates that the arch initially formed during the Laramide orogeny as part of a broad, north-south-trending uplift that extended from northwest Colorado into southern Wyoming and included the Rock Springs uplift. The axis of this structure was offset sinistrally and truncated by the late-Laramide uplift of the Uinta Mountains. This study examines available geologic, structure, Bouguer gravity, aeromagnetic, seismic, and paleomagnetic data to investigate this late-Laramide history, as well as indications of younger, post-Laramide tectonic events that have shaped the Douglas Creek arch and environs. This study also uses the existing data to evaluate the genetic relationships between Precambrian basement structures and shallower structures formed in the sedimentary cover. Results of this study suggest that a major east-west-oriented structure, the Douglas Creek fault, likely has a Precambrian ancestry and was reactivated during the Phanerozoic. Structures in the study area are consistent with periodic sinistral slip, dominantly along the Douglas Creek fault, most recently during late-Laramide tectonic events. Northwest-striking fractures flanking the Douglas Creek arch and extending into the surrounding basins are likely synthetic strike-slip faults related to a subsequent period of dextral slip on the Douglas Creek fault. This deformation could be the result of the northwest translation of the Colorado Plateau and opening of the Rio Grande rift during post-Laramide Tertiary extension. Wrench faulting has created enhanced permeability and numerous structural traps for petroleum accumulation across the Douglas Creek arch and in the surrounding basins. Wrench structures are identified by their distinct geometries, and the origins of their individual features can be discerned using supporting subsurface data. Knowledge of the genesis of the wrench system allows for better understanding of wrench structures and thus a better potential for success in the search for oil and gas.


ISSN: 1555-7332
EISSN: 1555-7340
Coden: WUGGAO
Serial Title: Rocky Mountain Geology
Serial Volume: 44
Serial Issue: 2
Title: Structural and tectonic evolution of the Douglas Creek Arch, the Douglas Creek fault zone, and environs, northwestern Colorado and northeastern Utah; implications for petroleum accumulation in the Piceance and Uinta Basins
Author(s): Bader, Jeffrey W.
Affiliation: AMEC Earth and Environmental, Honolulu, HI, United States
Pages: 121-145
Published: 200911
Text Language: English
Publisher: University of Wyoming, Dept. of Geology and Geophysics, Laramie, WY, United States
References: 63
Accession Number: 2010-009049
Categories: Structural geologyEconomic geology, geology of energy sources
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. strat. col., 1 table, geol. sketch maps
N37°00'00" - N41°00'00", W109°00'00" - W102°00'00"
N37°00'00" - N42°00'00", W114°04'60" - W109°04'60"
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute. Abstract, copyright, University of Wyoming. Reference includes data from GeoScienceWorld, Alexandria, VA, United States
Update Code: 201006
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