𝔖 Bobbio Scriptorium
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Sedimentation, cleavage and tectonic thinning in the aberystwyth grits between clarach and wallog, cardigan bay

✍ Scribed by Alan Wood


Book ID
102221788
Publisher
John Wiley and Sons
Year
2007
Tongue
English
Weight
438 KB
Volume
16
Category
Article
ISSN
0072-1050

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✦ Synopsis


Abstract

In recent years the folding and cleavage seen in the Aberystwyth Grits has been ascribed to downslope movement in soft unlithified sediment, not to tectonic forces. A detailed examination of folded beds in a small part of the outcrop was undertaken to test this theory. It is concluded that the folding and cleavage was initiated by movement from a rising tectonic ridge, but that the sediments may not have been completely lithified at the time of folding.