--> 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: Seismic Previous HitInterpretationNext Hit Validation by Previous HitFaultNext Hit Prediction and Fold Modeling

Schuman Wu, Robert Ratliff, Peter Geiser, Roy Kligfield

Computer programs have made seismic 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 seismic 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 Previous HitfaultNext Hit prediction and fold modeling. Whereas lithological boundaries are usually well-imaged on seismic profiles, the location of Previous HitfaultNext Hit discontinuities can be very imprecise. Previous HitFaultNext Hit prediction utilizes the deformed and assumed pre-faulting geometry of one or more hanging wall horizons and the connecting Previous HitfaultNext Hit segment to predict the remainder of the Previous HitfaultNext Hit geometry. In contrast, fold modeling uses a known or assumed Previous HitfaultNext Hit 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 Previous HitfaultNext Hit prediction and fold modeling. Seismic Previous HitinterpretationNext Hit using Previous HitfaultNext Hit prediction and/or fold modeling can quickly generate a via le cross section without using the iterative restoration process.

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

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