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KlepeisCIG2020.pptx (19.14 MB)
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KlepeisCIG2020.pptx

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conference contribution
posted on 20.07.2020, 15:13 by Keith A. Klepeis, Joshua J. Schwartz, Elena Miranda
The Fiordland and Stewart Island regions of SW New Zealand preserve a complete section of Cretaceous continental crust from depths of ~5 to ~65 km. These exposures allow us to directly observe how shear zone architecture and strain localization processes changed by depth within the crustal section.

Funding

NSF EAR 1119248

NSF EAR 1650219

NSF EAR 1352021

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Keywords

Shear zones, lower crust, strain localization, crustal structure

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CC BY 4.0

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