Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4687957 | Journal of Geodynamics | 2016 | 16 Pages |
Abstract
- Lithological nature of interplate boundary (subduction channel) from field analysis.
- Subduction channel is about 100-200Â m width at 10Â km depth.
- The Channel comprises blocks of lower (oceanic crust) and not upper compartments.
- Vertical veins opened by creep with local fluid, horizontal veins with deep fluid.
- Local fluid is 200 °C - deep fluid 300 °C (connected during co-seismic displacement).
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Marc Hässig, Yann Rolland, Marc Sosson, Ara Avagyan,