Abstract: The changing microstructural arrangement of graphite during deformation and hydrothermal alteration of amphibolite-facies mylonite, Alpine Fault, New Zealand. (2015 AGU Fall Meeting)

The changing microstructural arrangement of graphite during deformation and hydrothermal alteration of amphibolite-facies mylonite, Alpine Fault, New Zealand.

Martina Kirilova¹, Virginia Toy¹, Nick Timms², Dave Craw³, Timothy A Little⁴, Angela Halfpenny⁵ and Olivier Beyssac⁶, (1)University of Otago, Dunedin, New Zealand, (2)School of Earth and Planetary Science, Curtin University, Perth, Australia, (3)Department of Geology, University of Otago, P.O. Box 56, Dunedin, New Zealand, Dunedin, New Zealand, (4)Victoria University of Wellington, Wellington, New Zealand, (5)CSIRO Earth Science and Resource Engineering Perth, Perth, WA, Australia, (6)Institut de Minéralogie, de Physique des Matériaux et de Cosmochimie (IMPMC), Sorbonne Université, CNRS, MNHN, Paris, France

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