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

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.

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Cite this as

Stanislowski, Katja, Roesner, Alexander, Ikari, Matt J (2022). Dataset: Friction velocity dependence, cohesion, and XRD data of marine sediments from IODP Site U1301, Juan de Fuca plate. https://doi.org/10.1594/PANGAEA.940630

DOI retrieved: 2022

Additional Info

Field Value
Imported on November 29, 2024
Last update November 29, 2024
License CC-BY-4.0
Source https://doi.org/10.1594/PANGAEA.940630
Author Stanislowski, Katja
Given Name Katja
Family Name Stanislowski
More Authors
Roesner, Alexander
Ikari, Matt J
Source Creation 2022
Publication Year 2022
Resource Type application/zip - filename: Stanislowski-etal_2022
Subject Areas
Name: Geophysics

Related Identifiers
Title: Implications for megathrust slip behavior and pore pressure at the shallow northern Cascadia subduction zone from laboratory friction experiments
Identifier: https://doi.org/10.1016/j.epsl.2021.117297
Type: DOI
Relation: References
Year: 2022
Source: Earth and Planetary Science Letters
Authors: Stanislowski Katja , Roesner Alexander , Ikari Matt J .