G. J. Lensen
Abstract
Grabens and horsts between transcurrent faults in New Zealand, currently explained by normal faulting, are shown to be caused by lateral displacement. The mechanics of the formation of such features is explained.
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Grabens and horsts between transcurrent faults in New Zealand, currently explained by normal faulting, are shown to be caused by lateral displacement. The mechanics of the formation of such features is explained.
Key concepts: Horst, Graben, Horst and graben, Geology, Displacement (psychology), Fault (geology), Seismology, Tectonics