Low-grade metamorphism in granitoids and volcanic rocks, Cordillera Neuquina, Argentina
Granitoid and volcanic rocks of the Cordillera Neuquina between 38°45′ and 39°30′ south latitude have been metamorphosed under zeolite, prehnite-pumpellyite, and transitional greenschist facies conditions. This low-grade metamorphism is related to the circulation of hydrothermal solutions associated...
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| Autores principales: | Vattuone de Ponti, M.E., Latorre, C.O. |
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| Formato: | JOUR |
| Materias: | |
| Acceso en línea: | http://hdl.handle.net/20.500.12110/paper_08959811_v3_n4_p247_VattuonedePonti |
| Aporte de: |
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