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- W2247672785 abstract "Thrust faulting, folding, and penetrative compressional fabrics (e.g. spaced cleavage, pencils, and coal cleats) have been found in several outcrops within the central Deep River Basin (the southern Durham subbasin to the northern Wadesboro subbasin). The trend of these structures is nearly parallel to the basin, and may locally control the present geometry of the basin boundaries. These features are distributed throughout the stratigraphic section and across the entire width of the basin. In outcrops where relative timing can be determined, the compressional structures post-date all extensional and intrusive features associated with basin formation. In particular, thrusts cut across and displace basin-parallel normal faults and basin-normal cross-faults. All thrusts found to date verge northwest, and displacements of cross-fault boundaries indicate that transport was approximately 325[degree]." @default.
- W2247672785 created "2016-06-24" @default.
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- W2247672785 date "1994-03-01" @default.
- W2247672785 modified "2023-09-28" @default.
- W2247672785 title "Thrust faults and associated structures in the Deep River Basin: Evidence for post-extensional compression" @default.
- W2247672785 hasPublicationYear "1994" @default.
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