Tectonothermal analysis of high-temperature mylonitization in the
Mylonites in pelitic and quartzofeldsphatic gneisses from the Ouguela tectonic unit (Coimbra–Córdoba shear zone, SW Iberian Massif) have been studied as an example of high-temperature ductile deformation associated with transcurrent tectonics. Detailed microstructural and P–T analysis indicates that...
| Main Author: | |
|---|---|
| Other Authors: | , , |
| Format: | article |
| Language: | eng |
| Published: |
2011
|
| Subjects: | |
| Online Access: | http://hdl.handle.net/10174/2973 |
| Country: | Portugal |
| Oai: | oai:dspace.uevora.pt:10174/2973 |