Ar/Ar geochronology associated with fault reactivation in Fiordland
Klepeis, Keith A
Webb, Laura E
Blatchford, Hannah J
Schwartz, Joshua J
This is a 40Ar/39Ar geochrononology dataset from samples collected along transects across strain gradients associated with fault reactivation in Fiordland. The results have implications for Miocene-Pliocene fault reactivations in the upper plate of an incipient subduction zone at the Puysegur Margin of New Zealand. To understand the significance of the complex apparent age spectra (e.g. in light of cross-cutting relationships and other structural constraints), please see the full suite of integrated data presented in an accepted publication cited below.
How to cite this dataset:
Klepeis, K. A., Webb, L. E., Blatchford, H. J., Jongens, R., Turnbull, R., Schwartz, J. J., 2019. Ar/Ar geochronology associated with fault reactivation in Fiordland, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA). https://doi.org/10.1594/IEDA/111354.
DOI Creation Date:
Klepeis, K.A., Webb, L.E., Blatchford, H.J., Jongens, R., Turnbull, R., and Schwartz, J.J., The age and origin of Miocene-Pliocene fault reactivations in the upper plate of an incipient subduction zone, Puysegur Margin, New Zealand. Tectonics. Accepted August 2019.
Creative Commons Attribution-ShareAlike 4.0 International [CC-BY-SA-4.0]
University of Vermont Department of Geology Hawley and Mudge Awards
Coverage Scope: Regional (Continents, Oceans)
Geographic Location: Fiordland, New Zealand
User Contributed Keyword(s):
fault reactivation, pseudotachylyte, mylonite, resetting
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