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- W200882102 abstract "Abstract The Richmond and Taylorsville basins are Late Triassic to Jurassic(?) half-grabens which share a simple history displaying a tripartite division of sedimentary fill controlled by episodic tectonism. The basins formed by reactivation of the Hylas shear zone during initial rifting prior to the opening of the Atlantic Ocean. The first stage of deposition was dominated by active normal faulting and by debris flow and alluvial plain processes in the adjacent basins. Associated sedimentary rocks are mostly lithic conglomerates and sandstones. Tectonic activity was subdued during the second stage and the basins evolved into fluvial-lacustrine lowlands. Second-stage Taylorsville basin sediments were sand and mud deposited in oxbow lakes, perennial lakes, and meandering streams. Coal swamps developed in both basins, but apparently were more extensive in the Richmond basin than in the Taylorsville. Renewed tectonism more clearly defined a western border fault and initiated the third depositional stage when braided streams distributed sediments northward." @default.
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- W200882102 date "1988-01-01" @default.
- W200882102 modified "2023-09-27" @default.
- W200882102 title "Late Triassic depositional history of the Richmond and Taylorsville basins, Eastern Virginia" @default.
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- W200882102 doi "https://doi.org/10.1016/b978-0-444-42903-2.50022-1" @default.
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