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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1990
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| Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08959811_v3_n4_p247_VattuonedePonti http://hdl.handle.net/20.500.12110/paper_08959811_v3_n4_p247_VattuonedePonti |
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