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• W2028633980 abstract "The Alpine Fault of New Zealand forms the western boundary of a zone of distributed deformation formed by the oblique convergence of continental crust belonging to the Pacific and Australian plates. Structural and geodetic data from the Alpine Fault show that a large proportion of the total plate displacement is accommodated by rapid oblique slip on the fault. The remaining displacement is distributed over a 200 km wide zone to the east. The collision may be modelled as a two-sided deforming orogen, with the partitioning of deformation being controlled by erosional differences between the narrow high-strain inboard and broad low-strain outboard sides. In ancient collision zones, little evidence may remain of the nature and amount of displacement on the inboard side. Partitioning of deformation among pre-existing structures complicates interpretation of the outboard zone. Radiometric ages may post-date collision by several tens of millions of years and indicate slow isostatic uplift and unroofing. Collision ages, if preserved, may be recognized by high uplift rates calculated from muscovite-biotite pairs." @default.
• W2028633980 created "2016-06-24" @default.
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• W2028633980 creator A5037369643 @default.
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• W2028633980 date "1990-01-01" @default.
• W2028633980 modified "2023-10-17" @default.
• W2028633980 title "The obliquely-convergent plate boundary in the South Island of New Zealand: implications for ancient collision zones" @default.
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• W2028633980 doi "https://doi.org/10.1016/0191-8141(90)90084-c" @default.
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