Sea-level change and facies development across potential Triassic–Jurassic boundary horizons, SW Britain
The Late Triassic to Early Jurassic aged succession of SW Britain (the Penarth and lower Lias Groups) comprises mudstone, sandstone and limestone strata deposited in a variety of marine to non-marine environments. Faunal and floral characteristics of these successions have led to the proposal that o...
| Formato: | Journal article |
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Geological Society Publishing House
2004
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