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The AAPG/Datapages Combined Publications Database

AAPG Bulletin

Abstract

AAPG Bulletin, V. 89, No. 6 (June 2005), P. 781-797.

Copyright copy2005. The American Association of Petroleum Geologists. All rights reserved.

DOI:10.1306/0105052001108

Sandbox models of downward-steepening normal faults

Thomas L. Patton1

1BP America, 501 Westlake Park Boulevard, Houston, Texas 77079; [email protected]

ABSTRACT

Two deformational styles resulted from sandbox experiments examining the hanging-wall deformation above a downward-steepening normal-Previous HitfaultNext Hit bend comprised of two planar segments dipping at 40 and 60deg. In the first, hanging-wall layer-parallel extension dominated, with synthetic normal faults forming an upward-widening Previous HitfaultNext Hit-bound wedge above the Previous HitfaultNext Hit bend. Early forming, arcuate, vertical-to-reverse faults bound the wedge on its downthrown side and were followed by a planar, large-displacement synthetic normal Previous HitfaultNext Hit bounding the wedge on the upthrown side. This later Previous HitfaultNext Hit accommodated almost all of the subsequent displacement that occurred on the underlying 60deg Previous HitfaultNext Hit. Slip variably occurred along the 40deg segment of the Previous HitfaultNext Hit. Good analogs in nature exist for this deformation geometry. In the second deformational style, hanging-wall layer-parallel compression dominated, forming a monocline with antithetic hinge surfaces dipping downward to the Previous HitfaultNext Hit-bend surface. Antithetic reverse faults formed in the limb of the monocline. The upper hinge of the monocline intersected the footwall at the Previous HitfaultNext Hit bend, whereas its lower hinge intersected the 60deg Previous HitfaultNext Hit below the Previous HitfaultNext Hit bend. The lower hinge was older and formed near the location of the Previous HitfaultNext Hit bend prior to its being translated down the 60deg master Previous HitfaultTop as part of the hanging wall. Elements of this geometry correlate well with the results of some geometric-based numerical models, but strong analogs in nature are elusive.

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