Trench topography in subduction zones: A reflection of the plate decoupling depth
Subduction of lithospheric plates produces narrow, linear troughs (trench) in front of the overriding plates at the convergent boundaries. The trenches show a wide variation in their topographic characteristics, such as width, vertical depth, and bounding surface slopes. Benchmarking their controlli...
| Published in: | Frontiers in Earth Science |
|---|---|
| Main Authors: | , |
| Format: | Article |
| Language: | English |
| Published: |
Frontiers Media S.A.
2022-08-01
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| Subjects: | |
| Online Access: | https://www.frontiersin.org/articles/10.3389/feart.2022.908234/full |
