Sedimentation, cleavage and tectonic thinning in the aberystwyth grits between clarach and wallog, cardigan bay
作者:
Alan Wood,
期刊:
Geological Journal
(WILEY Available online 1981)
卷期:
Volume 16,
issue 1
页码: 57-64
ISSN:0072-1050
年代: 1981
DOI:10.1002/gj.3350160106
出版商: John Wiley&Sons Ltd
关键词: Submarine sliding;Transected folds;Shallow tectonics;Miogeanticlines;Aberystwyth;Greywackes
数据来源: WILEY
摘要:
AbstractIn 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.
点击下载:
PDF
(437KB)
返 回