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The AAPG/Datapages Combined Publications Database
AAPG Bulletin
Abstract
AAPG Bulletin, V.
DOI:10.1306/11250807130
Insights into the mechanisms of fault-related folding provided by volumetric structural restorations using spatially varying mechanical constraints
Chris A. Guzofski,1 Joachim P. Mueller,2 John H. Shaw,3 Pierre Muron,4 Donald A. Medwedeff,5 Frank Bilotti,6 Carlos Rivero7
1Department of Earth and Planetary Sciences, Harvard University, 20 Oxford Street, Cambridge, Massachusetts 02138; present address: Chevron, 1500 Louisiana St., Houston, Texas 77002; [email protected]
2Department of Earth and Planetary Sciences, Harvard University, 20 Oxford Street, Cambridge, Massachusetts 02138; present address: Chevron, 6001 Bollinger Canyon Rd., San Ramon, California 94583
3Department of Earth and Planetary Sciences, Harvard University, 20 Oxford Street, Cambridge, Massachusetts 02138
4Ecole Nationale Superieure de Geologie, Institut National Polytechnique de Lorraine/Centre de Recherches Petrographiques et Geochimiques, rue du Doyen Marcel Roubault, Nancy, 54500, France; present address: Chevron, 6001 Bollinger Canyon Rd., San Ramon, California 94583
5Chevron, 6001 Bollinger Canyon Rd., San Ramon, California 94583
6Unocal EE Technology, 14141 Southwest Fwy, Sugar Land, Texas 77478; present address: Chevron, 1500 Louisiana St., Houston, Texas 77002
7Unocal EE Technology, 14141 Southwest Fwy, Sugar Land, Texas 77478; present address: Chevron, 1500 Louisiana St., Houston, Texas 77002
ABSTRACT
We use a new, mechanically based volumetric structural restoration tool to investigate the mechanics of fault-related folding using natural examples imaged in three-dimensional (3-D) seismic data. The restoration technique is based on a finite element approach that simultaneously restores folding and faulting while allowing rock properties to spatially vary during restoration. We apply these techniques to two types of structures, detachment and shear fault-bend folds, where mechanical layering is a significant factor in their development. Our examples include a detachment anticline from the Caspian Sea and a shear fault-bend fold from the deep-water Niger Delta, both of which contain syntectonic growth horizons that help to constrain the restorations. Restorations of the detachment fold most closely match displacement fields specified in the kinematic forward models when materials are defined as incompressible and rigid, yet the variation of mechanical strength in restorations is perhaps more compatible with the growth of natural structures as recorded by syntectonic growth strata. This analysis shows that the restorations of the detachment fold favor a combination of both kink-band migration and limb rotation folding mechanisms. Numerical simulations of the growth shear fault-bend fold also closely match the displacement field prescribed by the kinematics of shear fault-bend fold models when weak basal units and bedding-plane slip surfaces, enabling flexural slip, are incorporated in the model. The results demonstrate that these techniques can be used to provide full 3-D restorations that closely match established two-dimensional kinematic theories, yet allow constraint of 3-D displacement fields and strain patterns in complex structures.
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