--> Seismic Interpretation Validation by Fault Prediction and Fold Modeling, by S. Wu, R. Ratliff, P. Geiser, and R. Kligfield; #90986 (1994).
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Abstract: Previous HitSeismicNext Hit Previous HitInterpretationNext Hit Validation by Fault Prediction and Fold Modeling

Schuman Wu, Robert Ratliff, Peter Geiser, Roy Kligfield

Computer programs have made Previous HitseismicNext Hit Previous HitinterpretationNext Hit validation a relatively easy and essential task for exploration/production geologists and geophysicists. Previous HitInterpretationNext Hit validation for contractional or extensional terranes is generally done by a restoration process using either a flexural slip algorithm, in which both bed-lengths and unit areas are preserved, or a vertical/oblique slip algorithm, in which only unit areas are conserved. The restoration procedure can reveal problems in a Previous HitseismicNext Hit Previous HitinterpretationNext Hit by unreasonable undeformed state geometries; corrections are usually done by modifying the deformed state Previous HitinterpretationNext Hit, followed by another restoration. This iteration is repeated until a satisfactory result is obtained.

Two useful alternative approaches to iterative restoration are fault prediction and fold modeling. Whereas lithological boundaries are usually well-imaged on Previous HitseismicNext Hit profiles, the location of fault discontinuities can be very imprecise. Fault prediction utilizes the deformed and assumed pre-faulting geometry of one or more hanging wall horizons and the connecting fault segment to predict the remainder of the fault geometry. In contrast, fold modeling uses a known or assumed fault trajectory to generate a kinematically valid hanging wall fold Previous HitinterpretationNext Hit. Depending on the nature of the problem, either flexural slip or vertical/oblique slip can be used for fault prediction and fold modeling. Previous HitSeismicNext Hit Previous HitinterpretationNext Hit using fault prediction and/or fold modeling can quickly generate a via le cross section without using the iterative restoration process.

An example of fault prediction and fold modeling using flexural-slip is presented for a Previous HitseismicNext Hit profile from the southern Appalachian fold-thrust belt. A series of Previous HitseismicNext Hit profiles across a Cenozoic basin in Northern China are used to extrapolate a 3D fault trajectory using vertical-slip fault prediction; the fault Previous HitinterpretationNext Hit and incremental deformation patterns predicted by fold modeling are corroborated by recent Previous HitseismicNext Hit event Previous HitdataTop.

AAPG Search and Discovery Article #90986©1994 AAPG Annual Convention, Denver, Colorado, June 12-15, 1994