ABSTRACT. The Coastal Batholith of south-central Chile between latitudes 33° and 40°S is composed of calc-alkaline granitoids emplaced in a relatively restricted time period. New SHRIMP U-Pb zircon ages on eight quartzdioritic to granitic rocks collected over a distance of 800 km yielded ages bet...
RESUMEN. El Batolito de la costa de Chile central-sur entre las latitudes 33° y 40°S se compone de granitoides calcoalcalinos y se ha emplazado en un período de tiempo relativamente restringido. Nuevas edades U-Pb SHRIMP en circones de ocho rocas graníticas a cuarzo-dioríticas, las que representa...
Enlace original:
http://repositorio.unab.cl/xmlui/handle/ria/2566
Deckart, Katja
,
Hervé, Francisco
,
Fanning, C. Mark
,
Ramírez, Valeria
,
Calderón, Mauricio
,
[U-Pb Geochronology and Hf-O Isotopes of zircons from the Pennsylvanian Coastal Batholith, South-Central Chile]
,
U-Pb Geochronology and Hf-O Isotopes of zircons from the Pennsylvanian Coastal Batholith, South-Central Chile
