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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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