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• W2004131012 abstract "Isopach maps and backstripped tectonic subsidence plots from the Triassic–Jurassic of the St. George’s Channel basin reveal significant departures from current models of extensional basin development: (i) rifting was highly protracted with discrete increments of crustal extension spanning ca. 120 My, (ii) substantial syn-kinematic sediment on the footwalls of major faults records pure shear (sub-seismic scale) deformation to have been important during regional Triassic extension. Forward modelling of depth-converted seismic interpretations is used to test the notion of combined pure and simple shear and to quantify the distribution of crustal extension between large and sub-seismic scale faults. The models indicate that Triassic subsidence was generated by ca. 2.5 km extension on major faults and 10 km extension by sub-seismic scale faulting. In fault-bounded compartments, Jurassic extension was dominated by large-scale faults, whereas in the areas of overlap between major fault segments, Jurassic extension was taken up chiefly by sub-seismic scale faulting. Comparison of measured vitrinite reflectance (VR) and VR modelled from heatflow history yielded by the forward models supports this scheme of episodic, pure shear-dominated extension. This research highlights the inherent difficulty in using seismic interpretation in isolation from quantitative subsidence and/or thermal history data to identify syn- and post-kinematic sedimentary sequences. Furthermore, it provides an opportunity to more fully reconstruct Mesozoic basin development in the West-of-UK area which, in the Cheshire, Central and East Irish Sea basins, is largely precluded by erosion of post-Triassic strata." @default.
• W2004131012 created "2016-06-24" @default.
• W2004131012 creator A5066557860 @default.
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• W2004131012 date "2000-06-01" @default.
• W2004131012 modified "2023-10-13" @default.
• W2004131012 title "Triassic–Jurassic development of the St. George’s Channel basin, offshore Wales, UK" @default.
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• W2004131012 doi "https://doi.org/10.1016/s0264-8172(00)00017-9" @default.
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