Reaction-induced rheological weakening enables oceanic plate subduction
Plate subduction initiation requires weak boundaries between tectonic plates, but how weaknesses develop is unclear. Here, using high-pressure friction experiments on peridotite gouge material, the authors show that hydration reactions contribute to the weak mantle shear zones leading to subduction...
| Main Authors: | , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Nature Publishing Group
2016-08-01
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| Series: | Nature Communications |
| Online Access: | https://doi.org/10.1038/ncomms12550 |