Publication Date:
2010-06-01
Description:
The Cretaceous Panther Tongue has an upward-coarsening and -thickening pattern and is well exposed in extensive large outcrops in the Book Cliffs area, west-central Utah. The deposits have been interpreted as having formed in a fluvial-dominated river delta environment that generated highly sediment-concentrated sustained (turbidity) flows during flooding, producing hyperpycnal-flow deposits on the delta front despite some resemblance to deep-water turbidites. The facies associations indicate terminal distributary channel, channel mouth, and proximal delta-front and distal delta-front depositional environments. The measured paleocurrents indicate a south-southwest transport of the sediments. The thickness of the hyperpycnal sandstone beds ranges from centimeters to meters. Sandstones are characteristically parallel laminated, sometimes structureless or rarely display inclined strata of cut-and-fill type. The sandstone hyperpycnal beds dominate the delta-front clinoforms and dip southward, consistent with the other paleocurrent indicators. Individual sandstone beds in the clinoforms have dips that range from 0.1° on the distal delta front (lower part of the outcrops) to 3° in the proximal parts (upper part of the outcrops). The hyperpycnal beds can be traced from a proximal mouth-bar environment to the distal delta front over a distance of hundreds of meters. As individual beds extend from mouth bar to distal delta-front environments, they become systematically finer grained and thinner. Over short distances (hundreds of meters), the beds thin with rates ranging between 0.0001 (i.e., dm/km) to 0.02 (i.e., tens of meters per kilometer). The sandstone beds thin to a greater degree in a dip direction than along strike, indicating a relatively strike-elongate (flow-normal) geometry of the hyperpycnal flows and of the delta lobes. The wider than longer geometry of the delta-front beds requires that reservoir development be more focused upon the downdip facies changes (heterogeneities) than the lateral (along strike) heterogeneities. Cornel Olariu is a research associate at the University of Texas. He earned a geology engineering degree in 1995 from the University of Bucharest, and an M.S. degree in 2002 and a Ph.D. in 2005 both in geological sciences from the University of Texas at Dallas. He is interested in clastic sedimentology with focus on shallow-water depositional systems and more specifically on mechanisms of sediment transfer from shallow to deep water. Ronald J. Steel is a professor and Davis Centennial Chair at the University of Texas at Austin. He received his B.Sc. degree in 1967 and his Ph.D. in 1971 from the University of Glasgow, United Kingdom. His research is aimed primarily at using clastic sedimentology to address problems in basin analysis and particularly to decipher the signatures of tectonics, sea level change, and sediment supply in stratigraphic successions. Andrew L. Petter is a Ph.D. candidate in the Jackson School of Geosciences, University of Texas at Austin. He earned a B.S. degree in geology from Rice University in 2002 and an M.S. degree in geological sciences from the University of Texas at Austin in 2005. He is currently studying the partitioning of sediment across alluvial, deltaic, and shelf-margin systems using numerical models, flume experiments, and outcrop and subsurface data.
Print ISSN:
0149-1423
Electronic ISSN:
1943-2674
Topics:
Geosciences
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