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The AAPG/Datapages Combined Publications Database

GCAGS Transactions

Abstract


Gulf Coast Association of Geological Societies Transactions
Vol. 38 (1988), Pages 579-579

Abstract: Variation of "Growth Fault" Structural Styles in the Texas Gulf Coast Basin

Thomas E. Ewing (1)

ABSTRACT

Within the overall theme of Gulf Coast growth Previous HitfaultingNext Hit there is significant regional variability. Detailed mapping and regional seismic interpretation of selected areas in growth fault trends of onshore Texas point up this variability, which can be related to patterns of oil and gas fields and overpressure occurrence.

Several basic styles of growth Previous HitfaultingNext Hit are observed in the Tertiary sequence of the Texas Gulf Coast. The most distinctive are glide-fault systems, which display a basal detachment below highly faulted and rotated, usually sand-rich and hydrocarbon-bearing strata. Most glide systems show rapidly migrating highs following the basal detachment, an "escalator" model (Vicksburg, Sarita, Corsair). However, others involve domino-style extension similar to Great Basin models (Yegua, Lobo). Other areas show rotated blocks on listric faults which may sole into a deep slide plane at great depth (Frio), often downdip of ridges of mobile shale (Zapata Wilcox). Still other growth faults are only slightly listric, have slight block rotations, and may root at great depth (Dewitt Wilcox). More local growth Previous HitfaultingNext Hit also occurs along the margins of salt- or shale-withdrawal basis, or as compactional Previous HitfaultingNext Hit related to shale ridges.

Factors that control structural styles must include: the nature of the pre-progradation substrate; presence of salt- or shale-related bathymetric features on the old continental slope; the rate and spatial variation of sediment loading; and the relative excess of sedimentation over subsidence. Presence of thick mud sequences in the substrate favors shale-ridge development and glide-fault systems. Slope features localize the trend of Previous HitfaultingNext Hit and may concentrate it over the slip-face of the slope feature. The spatial variance of sedimentation may determine the geometry of Previous HitfaultingTop, and also initiate salt or shale movement. The relative excess of sedimentation over subsidence determines the magnitude and timing of the fault systems.

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ACKNOWLEDGMENTS AND ASSOCIATED FOOTNOTES

(1) Frontera Exploraton Services, 900 NE Loop 410, San Antonio, TX 78209

Copyright © 1999 by The Gulf Coast Association of Geological Societies