Sedimentary structures associated with extensional fault movement from the Westphalian of NE England
- 1 January 1987
- journal article
- Published by Geological Society of London in Geological Society, London, Special Publications
- Vol. 28 (1), 511-516
- https://doi.org/10.1144/gsl.sp.1987.028.01.33
Abstract
Although differential subsidence and extension has been well established as a control on sedimentation for the Dinantian of N England, the continuation of this tectonic regime into Silesian times is less well demonstrated.Keywords
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