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- W2054155841 abstract "The geometry of beds in the volume surrounding a single blind planar fault depends on: (i) the axial ratio of the fault surface ellipse, (ii) the ratio between the maximum displacement and the maximum dimension of the fault surface, (iii) the displacement distribution on the fault surface from the point of maximum displacement to zero displacement at the tip-line loop (fault surface displacement profile) and (iv) the rate at which the displacement decreases to zero along a normal to the fault surface (reverse drag displacement profile). These relationships, which are either known or can be estimated, are incorporated in a computer model which generates structural contours on horizons intersected by a planar fault. Structural contour patterns also vary with the pre-faulting dip and strike of beds, the dip and strike of the fault and the level at which a bed intersects the fault surface. When the boundary conditions are relaxed to include synsedimentary faults, the ratio of hangingwall to footwall displacement varies systematically with fault dip.A synthetic structural contour map is matched with that of an actual fault. Model isopachs, based on simple depositional models, are generated for synsedimentary units. Cross-sections are generated for synsedimentary faults by sequential fault growth and sedimentary deposition, and show features similar to actual cross-sections. The soft-domino model is applicable primarily to dip-slip tectonic faults with maximum displacements of up to about 5 km; listric faults are not considered." @default.
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- W2054155841 date "1989-01-01" @default.
- W2054155841 modified "2023-10-09" @default.
- W2054155841 title "Modelling of bed contours and cross-sections adjacent to planar normal faults" @default.
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- W2054155841 doi "https://doi.org/10.1016/0191-8141(89)90071-0" @default.
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