Shear Zone Development in Serpentinized Mantle: Implications for the Strength of Oceanic Transform Faults

Author:

Cox Sophie1ORCID,Fagereng Åke1ORCID,MacLeod Christopher J.1ORCID

Affiliation:

1. School of Earth and Environmental Sciences Cardiff University Cardiff UK

Funder

H2020 European Research Council

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference107 articles.

1. Earthquake slip on oceanic transform faults

2. Generation and propagation of G waves from the Niigata Earthquake of June 16, 1964. Part 2. Estimation of earthquake movement, released energy, and stress‐strain drop from the G wave spectrum;Aki K.;Bulletin of the Earthquake Research Institute, University of Tokyo,1966

3. Deformation mechanisms and rheology of serpentines in experiments and in nature

4. Development of schistosity by dissolution–crystallization in a Californian serpentinite gouge

5. Variable coupling across weak oceanic transform fault: Flateyjarskagi, Iceland

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