British Triassic fossil reptile sites

作者: M. J. Benton , P. S. Spencer

DOI: 10.1007/978-94-011-0519-4_4

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摘要: The British Triassic deposits have a broad Ushaped outcrop in the English Midlands, with continuation south-westwards to south Wales and Devon (Figure 4.1). Smaller outcrops occur northwest England, Northern Ireland Scotland (Warrington et al., 1980, figs 2 3). sediments are almost wholly continental ter restrial red-beds deposited fault-bounded basins southern western Britain on more regionally subsiding Eastern England Shelf, which formed onshore marginal part of Southern North Sea Basin (Audley-Charles, 1970; Holloway, 1985). In Late Permian Early Triassic, renewed extensional subsidence Wessex Basin, Worcester Graben Needwood Cheshire basins, resulted establishment an axial drainage system flowed northwards from Variscan Highlands (Holloway,

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