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Age and Sr isotopic composition of volcanic rocks in the Maricunga Belt, Chile: implications for magma sources

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Age and Sr isotopic composition of volcanic rocks in the Maricunga Belt, Chile: implications for magma sources; 1994; Article; Journal; Journal of South American Earth Sciences; McKee, E. H.; Robinson, A. C.; Rybuta, J. J.; Cuitino, L.; Moscoso, R. D.

Summary

K-Ar and 40Ar/39Ar dating of volcanic rocks from the Maricunga belt of north-central Chile indicate that igneous activity took place throughout most of Miocene time at various places in the 150 by 30 km belt. No migration patterns of volcanism appear in the Miocene rocks of the belt. Volcanic activity ceased by the end of the Miocene. All the Miocene volcanic rocks studied are calcic andesites to dacites with about 62% SiO2, 18% A12O3, 4% Fe2O3 (total), and 2% K2O. Initial 87Sr/86Sr (Sri) values fall into two groups, one of lower values around 0.7050 to the west and the other of higher values around 0.7060 to the east. It is postulated that the two Sri groups reflect two adjoining coherent lower-crustal magma sources of possibly different [...]

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local-index unknown 70017077
local-pk unknown 70017077
series unknown Journal of South American Earth Sciences

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citationTypeArticle
journalJournal of South American Earth Sciences
languageEnglish
parts
typevolume
value7
typeissue
value2

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