New Zealand Journal of Geology and Geophysics | Vol.1, Issue.3 | | Pages 533-540
Note on the compressional angle between intersecting transcurrent clockwise and anti-clockwise faults
Summary It is shown that the compressional angle between intersecting major transcurrent clockwise and anti-clockwise faults is acute in tensional, and obtuse in compressional regions.
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Note on the compressional angle between intersecting transcurrent clockwise and anti-clockwise faults
Summary It is shown that the compressional angle between intersecting major transcurrent clockwise and anti-clockwise faults is acute in tensional, and obtuse in compressional regions.
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