Friction of hornblende and tremolite at hydrothermal conditions with low effective normal stress and high pore pressure

Author:

Liu Yang,He Changrong

Funder

National Natural Science Foundation of China

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference48 articles.

1. Controls on the rheological properties of peridotite at a palaeosubduction interface: a transect across the base of the Oman–UAE ophiolite;Ambrose;Earth Planet. Sci. Lett.,2018

2. The solubility of quartz in supercrtical water;Anderson;Am. J. Sci.,1965

3. Probing the transition between seismically coupled and decoupled segments along an ancient subduction interface;Angiboust;Geochem. Geophys. Geosyst.,2015

4. A rate-, state-, and temperature-dependent friction law with competing healing mechanisms;Barbot;J. Geophys. Res. Solid Earth,2022

5. The stabilizing effect of high pore-fluid pressure along subduction megathrust faults: Evidence from friction experiments on accretionary sediments from the Nankai Trough;Bedford;Earth Planet. Sci. Lett.,2021

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