Late Jurassic and mid-Teritiary brittle-ductile deformation in the Opodepe region, Sonora, Mexico
In central Sonora, in the Opodepe region, regional strike-slip foliation in Proterozoic rocks is the result of Middle to Late Jurassic shearing, whereas extensional structures in Paleogene plutons correspond to the evolution of mid-crustal extension during Middle Tertiary… in order to continue, dow...
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| Format: | Article |
| Language: | English |
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Universidad Nacional Autónoma de México
2019-01-01
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| Series: | Revista Mexicana de Ciencias Geológicas |
| Subjects: | |
| Online Access: | https://rmcg.unam.mx/index.php/rmcg/article/view/1134 |
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