Rate-and-state friction parameters from core sample C0002T-2K1, IODP Expedition 358

DOI

We tested an intact sample from Borehole C0002T, recovered from the inner accretionary prism at the Nankai Trough, at estimated in-situ effective stress conditions in a laboratory friction experiment to measure its strength and frictional characteristics. We use inverse modeling within the rate-and-state dependent friction framework to extract parameters used to calculate various estimates of the critical patch length for frictional instability. This study reports new analyses in addition to those reported from the same sample by Okuda et al., 2021.

Identifier
DOI https://doi.pangaea.de/10.1594/PANGAEA.973996
Related Identifier IsDerivedFrom https://doi.org/10.1029/2021JB022546
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.973996
Provenance
Creator Ikari, Matt J (ORCID: 0000-0002-8164-411X)
Publisher PANGAEA
Publication Year 2025
Funding Reference European Research Council https://doi.org/10.13039/501100000781 Crossref Funder ID 714430 https://cordis.europa.eu/project/id/714430 Plate-rate experimental deformation: Aseismic, transient or seismic fault slip
Rights Creative Commons Attribution 4.0 International; Data access is restricted (moratorium, sensitive data, license constraints); https://creativecommons.org/licenses/by/4.0/
OpenAccess false
Representation
Resource Type Bundled Publication of Datasets; Collection
Format application/zip
Size 8 datasets
Discipline Earth System Research
Spatial Coverage (136.637 LON, 33.308 LAT)