| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4699032 | Chemical Geology | 2013 | 13 Pages |
Abstract
⺠High-velocity friction experiments demonstrate coseismic serpentine dehydration. ⺠Serpentine dehydration was caused by both the friction heating and heat diffusion. ⺠FTIR and TG-DSC analyses show that all water in the slipping zone was released. ⺠Rapid thermal pressurization led to a pronounced weakening of seismic fault zone.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Aiming Lin, Soichiro Takano, Tetsuro Hirono, Kyuichi Kanagawa,