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- W76154343 abstract "Abstract Four rift basins are buried on the Long Island platform of the U.S. Atlantic continental margin. The basins are characterized by tilted, subparallel reflectors landward of the basement hinge zone and a wedge-shaped reflector geometry seaward of the hinge zone. The change in reflector geometry across the hinge zone is a function of differential erosion in response to uplift landward of and greater subsidence seaward of the hinge. A qualitative two-stage model of rift evolution explains these changes: an early stage characterized by widespread half-graben formation along listric or planar normal faults and a late stage characterized by uplift and erosion at and landward of the hinge. Age control in the offshore region is poor, but comparison with theoretical models of rift formation places the most probable age of uplift during the end of rifting or early drifting, although our data cannot distinguish between possible mechanisms of uplift. On the western end of the Long Island platform, rift basins may have formed by extension along the edge of a buried detachment surface; in the central platform, they appear to have formed by extension along (antithetic?) pairs of faults that penetrate the crust." @default.
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- W76154343 date "1988-01-01" @default.
- W76154343 modified "2023-09-26" @default.
- W76154343 title "Evolution of rift basins on the continental margin off southern New England" @default.
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- W76154343 doi "https://doi.org/10.1016/b978-0-444-42903-2.50009-9" @default.
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