Conodont geothermometry of the lower Paleozoic from the Precordillera (Cuyania terrane), northwestern Argentina

The thermal history of the Precordillera terrane of northwestern Argentina has been constrained by the conodont colour alteration index (CAI) in combination with previously published paleothermal data (e.g., illite crystallinity and clay mineral assemblages). The pattern of paleotemperatures display...

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Autores principales: Voldman, G.G., Albanesi, G.L., Ramos, V.A.
Formato: JOUR
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_08959811_v29_n2_p278_Voldman
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