--> Abstract: Influence of Subaqueous Shelf Angle on Coastal Plain-Shelf-Slope Deposits Resulting from a Rise or Fall in Base-Level, by L. J. Wood, F. G. Ethridge, and S. A. Schumm; #91004 (1991)

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Influence of Subaqueous Shelf Angle on Coastal Plain-Shelf-Slope Deposits Resulting from a Rise or Fall in Base-Level

WOOD, LESLI J., F. G. ETHRIDGE, and S. A. SCHUMM, Colorado State University, Fort Collins, CO

Extensive research in the past decade concerning the effects of base-level fluctuations on coastal plain-shelf-slope systems along passive margins has failed to properly assess the influence of the subaqueous shelf angle on the development, character, and preservation of the resulting deposits. A series of experiments were performed in a 4 m by 7 m flume to examine the effect that differing shelf angles have on a simulated coastal plain-shelf-slope system undergoing a cycle of base-level rise and fall.

Results of the experiments indicate that the angle of the shelf affects (1) the amount of sediment available for deposition, (2) the timing of the influx of drainage basin sediment into the lower portions of the fluvial system, and (3) the width to depth ratio and sinuosity of fluvial systems that develop on the shelf. Base-level fall over a steep shelf results in deep, narrow, straight fluvial channels on the shelf and fine-grained, thick shelf-margin deltas. Depositional systems show high sedimentation rates, but a low ratio of coarse-grained to fine-grained sediment. Multiple fluvial incisions on the shelf are rapidly abandoned for a single incised valley. During subsequent base-level rise, deposits are well preserved owing to their thickness and the rapid rate at which the transgr ssion occurs.

In contrast, gentle shelf angles result in shallow, wide, meandering fluvial channels on the shelf and coarser-grained, thinner shelf-margin deltas. Depositional systems have a lower sedimentation rate, but a high ratio of coarse-grained to fine-grained sediment. Multiple fluvial incisions on the shelf are active for a longer period of time. During subsequent base-level rise, deposits have a low potential for preservation owing to their thin nature and the slower rate at which transgression occurs over the shelf.

 

AAPG Search and Discovery Article #91004 © 1991 AAPG Annual Convention Dallas, Texas, April 7-10, 1991 (2009)