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The AAPG/Datapages Combined Publications Database
Southeast Asia Petroleum Exploration Society (SEAPEX)
Abstract
Styles of Compressional Wrench Faulting Taranaki Basin, New Zealand
Abstract
Formation of the Taranaki Basin was initiated in the Late Cretaceous in response to the break-up of Gondwanaland. The Indo-Pacific plate boundary propagated through New Zealand from the mid Paleogene. Four structural styles resulted from two phases of Neogene, compressional wrench faulting. Wrenching resulted from the reactivation of pre-existing faults when these faults were subjected to shear stress derived directly from the Alpine Fault.
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