Articles | Volume 10, issue 4
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, Steven A. F. Smith, James M. Scott, Jeremy S. Rooney, Cecilia Viti, and Keith C. Gordon


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
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)
AR by Matthew Tarling on behalf of the Authors (14 Jun 2019)  Manuscript 
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.