The effect of obliquity on temperature in subduction zones: insights from 3-D numerical modeling
The geotherm in subduction zones is thought to vary as a function of the subduction rate and the age of the subducting lithosphere. Along a single subduction zone the rate of subduction may strongly vary due to changes in the angle between the trench and the plate convergence vector, i.e., the s...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2018-06-01
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| Series: | Solid Earth |
| Online Access: | https://www.solid-earth.net/9/759/2018/se-9-759-2018.pdf |