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Structure, late Quaternary slip rate and earthquake potential of marine reverse faults along the North Westland deformation front, New Zealand

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Title
Structure, late Quaternary slip rate and earthquake potential of marine reverse faults along the North Westland deformation front, New Zealand
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FigShare
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FigShare
Description

The North Westland deformation front runs offshore for 320 km between Cape Farewell and Hokitika at a distance of 3–30 km from the coast. From marine seismic reflection profiles integrated with published sediment core and coastal uplift data, we infer late Quaternary activity on six major reverse faults. The principal structures are the Cape Foulwind, Kahurangi and Kongahu faults and the newly named Farewell, Elizabeth and Razorback faults. They include Late Cretaceous and Paleogene rift faul...

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Date created
09 May, 2016
Creator
PM Barnes / FC Ghisetti
URL
https://doi.org/10.6084/m9.figshare.3362683
Related subjects
Active faults / compressional inversion / folding / New Zealand / North Westland / Quaternary stratigraphy / seismic hazard / South Island / Biophysics / Evolutionary Biology / Environmental Sciences not elsewhere classified / Ecology / Biological Sciences not elsewhere classified / Marine Biology / Inorganic Chemistry

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