Friction velocity dependence, cohesion, and XRD data of marine sediments from IODP Site U1301, Juan de Fuca plate

DOI

To investigate the lithostratigraphic position and frictional behavior of the shallow plate boundary fault at the northern Cascadia subduction zone, we conducted laboratory friction experiments on sediments recovered at IODP Site U1301. We used a single-direct shear device under room temperature conditions with 3.5% simulated seawater to perform cohesion tests, plate rate tests and velocity step tests (VST). Friction data from VSTs were inversly modelled to obtain rate- and state friction (RSF) parameters.

Identifier
DOI https://doi.org/10.1594/PANGAEA.940630
Related Identifier IsSupplementTo https://doi.org/10.1016/j.epsl.2021.117297
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.940630
Provenance
Creator Stanislowski, Katja ORCID logo; Roesner, Alexander ORCID logo; Ikari, Matt J (ORCID: 0000-0002-8164-411X)
Publisher PANGAEA
Publication Year 2022
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; https://creativecommons.org/licenses/by/4.0/
OpenAccess true
Representation
Resource Type Bundled Publication of Datasets; Collection
Format application/zip
Size 3 datasets
Discipline Earth System Research
Spatial Coverage (-127.763W, 47.755S, -127.763E, 47.755N)