Thermochronological evidence of a low-angle, mid-crustal detachment plane beneath the central South Island, New Zealand
Author:
Affiliation:
1. School of Geography, Environment and Earth Sciences; Victoria University of Wellington; Wellington New Zealand
2. GNS Science, Lower Hutt; New Zealand
3. Institute of Earth Sciences, University of Lausanne; Lausanne Switzerland
Funder
Marsden Fund
Doctoral Scholarship and Faculty of Science Research
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1002/2016GC006402/fullpdf
Reference84 articles.
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3. Width of mantle deformation across a continental transform: Evidence from upper mantle (Pn) seismic anisotropy measurements;Baldock;Geology,2005
4. Strike-slip structure and sedimentary basins of the southern Alpine Fault, Fiordland, New Zealand;Barnes;Geol. Soc. Am. Bull.,2005
5. Scale dependence of oblique plate-boundary partitioning: New insights from LiDAR, central Alpine fault, New Zealand;Barth;Lithosphere,2012
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