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Summary
| Description |
English: (1a,b) shows magma generation in a transpressional environment at the restraining bend in a strike slip fault. Magma here is generated via compressional partial melting of the thickened crustal rock. (2a,b) shows magma generation in a transtensional environment in the releasing bend of a strike-slip fault via crustal thinning and decompression melting. |
| Date | |
| Source | Own work |
| Author | Jasmineforshaw |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 09:21, 13 November 2023 | | 2,464 × 2,266 (442 KB) | Jasmineforshaw | Uploaded own work with UploadWizard |
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