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- W2011261316 abstract "The depositional setting for the Greenbrier Limestone of the central Appalachian basin included a continually subsiding basin, centered in southeastern West Virginia and adjacent Virginia, separated by a hinge zone from a broad shallow shelf located to the north and northwest. Oolitic limestones are thick and extensive in southern West Virginia; however, most of these units thin drastically and change in lithology to the north. An area of uplift, the West Virginia dome, developed along the hinge zone in north-central West Virginia. During early Greenbrier deposition, this area was exposed as an island. Later, the dome was submerged but remained as a submarine high throughout Greenbrier sedimentation. The northernmost occurrences of Mississippian oolitic limestones in West Virginia surround this feature." @default.
- W2011261316 created "2016-06-24" @default.
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- W2011261316 date "1989-01-01" @default.
- W2011261316 modified "2023-09-26" @default.
- W2011261316 title "Drowning of an Ooid Shoal: Mississippian Greenbrier Limestone Near West Virginia Dome: ABSTRACT" @default.
- W2011261316 doi "https://doi.org/10.1306/44b4a311-170a-11d7-8645000102c1865d" @default.
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