Laboratory friction measurements of the Alpine Fault, New Zealand

DOI

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).

Identifier
DOI https://doi.org/10.1594/PANGAEA.918375
Related Identifier IsSupplementTo https://doi.org/10.1007/s00531-014-1115-5
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.918375
Provenance
Creator Ikari, Matt J (ORCID: 0000-0002-8164-411X)
Publisher PANGAEA
Publication Year 2020
Rights Creative Commons Attribution 4.0 International; https://creativecommons.org/licenses/by/4.0/
OpenAccess true
Representation
Resource Type Publication Series of Datasets; Collection
Format application/zip
Size 3 datasets
Discipline Earth System Research
Spatial Coverage (170.325 LON, -43.316 LAT)