Articles | Volume 10, issue 4
Solid Earth, 10, 1025–1047, 2019
https://doi.org/10.5194/se-10-1025-2019
Solid Earth, 10, 1025–1047, 2019
https://doi.org/10.5194/se-10-1025-2019
Research article
04 Jul 2019
Research article | 04 Jul 2019

The internal structure and composition of a plate-boundary-scale serpentinite shear zone: the Livingstone Fault, New Zealand

Matthew S. Tarling et al.

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AR by Matthew Tarling on behalf of the Authors (12 Jun 2019)  Author's response    Manuscript
ED: Publish as is (12 Jun 2019) by Cristiano Collettini
ED: Publish as is (12 Jun 2019) by Federico Rossetti(Executive Editor)
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Short summary
Shear zones dominated by hydrated mantle rocks (serpentinites) occur in many tectonic settings around the world. To better understand the internal structure, composition and possible mechanical behaviour of these shear zones, we performed a detailed field, petrological and microanalytical study of the Livingstone Fault in New Zealand. We propose a conceptual model to account for the main physical and chemical processes that control deformation in large serpentinite shear zones.