Some theoretical structures associated with transcurrent faulting applied to the alpine fault
作者:
J. C. Schofield,
期刊:
New Zealand Journal of Geology and Geophysics
(Taylor Available online 1960)
卷期:
Volume 3,
issue 3
页码: 461-466
ISSN:0028-8306
年代: 1960
DOI:10.1080/00288306.1960.10422088
出版商: Taylor & Francis Group
数据来源: Taylor
摘要:
During transcurrent faulting arcuate fold trends are produced and the regional stress is resolved into a series of oblique, lower order, stress systems which enable cross folds to develop without any necessary changes to the direction of the regional stress.
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