Conodont palaeothermometry of contact metamorphism in Middle ordovician rocks from the precordillera of western Argentina
The Yerba Loca Formation (Middle-Upper Ordovician), exposed in the Western Precordillera, San Juan, Argentina, is made up of clastic-carbonate turbidites, and basic-ultrabasic rocks. It is affected by regional Siluro-Devonian very low-grade metamorphism that locally reaches greenschist facies. At An...
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| Autores principales: | Voldman, G.G., Albanesi, G.L., Do Campo, M. |
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| Formato: | JOUR |
| Materias: | |
| Acceso en línea: | http://hdl.handle.net/20.500.12110/paper_00167568_v145_n4_p449_Voldman |
| Aporte de: |
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