Laboratory friction measurements of the Alpine Fault, New Zealand

doi:doi:10.1594/PANGAEA.918375

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Laboratory friction measurements of the Alpine Fault, New Zealand

We use laboratory shearing experiments to smeasure the frictional properties of fault related rocks and their precursors depending on the lithology, presence of pore fluid, effective normal stress, and temperature. Conditions are appropriate for the surface to several kilometres depth on the Alpine Fault (from 50-100 MPa, 22-160 °C, fluid-saturated).

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Cite this as

Ikari, Matt J (2020). Dataset: Laboratory friction measurements of the Alpine Fault, New Zealand. https://doi.org/10.1594/PANGAEA.918375

DOI retrieved: 2020

Additional Info

Field	Value
Imported on	November 30, 2024
Last update	November 30, 2024
License	CC-BY-4.0
Source	https://doi.org/10.1594/PANGAEA.918375
Author	Ikari, Matt J
Given Name	Matt J
Family Name	Ikari
Source Creation	2020
Publication Year	2020
Resource Type	application/zip - filename: Ikari-etal_2015
Subject Areas	Name: Lithosphere
Related Identifiers	Title: Shear behavior of DFDP-1 borehole samples from the Alpine Fault, New Zealand, under a wide range of experimental conditions Identifier: https://doi.org/10.1007/s00531-014-1115-5 Type: DOI Relation: References Year: 2015 Source: International Journal of Earth Sciences Authors: Ikari Matt J , Trütner S , Carpenter Brett M , Kopf Achim J .