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Title: Laramide tectonics and humid alluvial fan sedimentation, Ne Uinta uplift, Utah and Wyoming

Journal Article · · Journal of Sedimentary Petrology; (United States)
OSTI ID:6383847
;  [1]
  1. Colorado State Univ., Fort Collins (United States)

This paper describes and interprets a sequence of syntectonic conglomerates and sandstones shed from the northeast flank of the Uinta Mountains during an early Eocene phase of the Laramide orogeny. The study area centers around a cuesta 10 km long known as Richards Mountain located on the Utah-Wyoming border about 3 km north of the Uinta fault zone. Conglomerates and sandstones of the basal Wasatch Formation that crop out on Richards Mountain constitute an exhumed, strike-parallel deposit of carose sediments that formed adjacent to the rising Uinta Mountains uplift. These rocks are an example of sedimentation in a proximal, humid piedmont setting and provide clues to the relative rate and timing of a major cycle of uplift and erosion of the Uinta Mountains. Topics specifically addressed in this study include: (1) sedimentary facies, fluvial architecture, depositional processes, paleocurrents, and grain-size trends at Richards Mountain, based on detailed measured sections; (2) tectonic significance of the richards Mountain sequence, including tectonic and geomorphic explanations for several scales of cyclicity within the sequence; and (3) Early Paleogene tectonic and depositional history of the northeastern flank of the Uinta Uplift and the southern Green River Basin.

OSTI ID:
6383847
Journal Information:
Journal of Sedimentary Petrology; (United States), Vol. 63:3; ISSN 0022-4472
Country of Publication:
United States
Language:
English