Fault–fracture mesh development produces tectonic tremor in fluid-overpressured serpentinized mantle wedge
Abstract Deep tectonic tremor occurs repeatedly at the base of a forearc mantle wedge corner, where a highly fluid-pressurized serpentinite shear zone is thought to develop. However, the deformation mechanisms that accommodate these tremors within the shear zone remain unclear. Here, we present obse...
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| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Nature Portfolio
2025-03-01
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| Series: | Communications Earth & Environment |
| Online Access: | https://doi.org/10.1038/s43247-025-02159-7 |
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