Basins and swells and the evolution of an epeiric sea (pliensbachian-bajocian of Great Britain)

During Pliensbachian-Bajoeian times northern Europe, including Britain, was covered by an epeiric sea. Sediments formed include clays sandstones, limestones and ironstones, usually cyclically arranged; different facies were developed synchronously in different areas. There is very little evidence, b...

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Bibliographic Details
Main Authors: Sellwood, B, Jenkyns, H
Format: Journal article
Language:English
Published: 1975