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Zircon Trace Element and O-Hf Isotope Analyses of Mineralized Intrusions from El Teniente Ore Deposit, Chilean Andes: Constraints on the Source and Magmatic Evolution of Porphyry Cu-Mo Related Magmas
| Indexado |
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| DOI | 10.1093/PETROLOGY/EGS010 | ||||
| Año | 2012 | ||||
| Tipo | artículo de investigación |
Citas Totales
Autores Afiliación Chile
Instituciones Chile
% Participación
Internacional
Autores
Afiliación Extranjera
Instituciones
Extranjeras
Abstract
At the time of El Teniente formation, dehydration melting occurred coevally with arc migration, which probably influenced the fertility of the magmas by increasing the melt component derived from this process relative to the component derived from primary basalt differentiation. At a regional scale, such reactions are expected to occur as a consequence of progressive crustal thickening during the constructive period of the Andes, and can explain the simultaneous generation of porphyry deposits in the Miocene-Pliocene Cu-Mo belt of Central Chile.
| Ord. | Autor | Género | Institución - País |
|---|---|---|---|
| 1 | MUNOZ-MORALES, MAURICIO ERNESTO | Mujer |
Universidad de Chile - Chile
|
| 2 | CHARRIER-GONZALEZ, REYNALDO | Hombre |
Universidad de Chile - Chile
|
| 3 | Fanning, C. Mark | Hombre |
Australian Natl Univ - Australia
Australian National University - Australia The Australian National University - Australia |
| 4 | Maksaev, V. | Hombre |
Universidad de Chile - Chile
|
| 5 | Deckart, K. | Mujer |
Universidad de Chile - Chile
|
| Fuente |
|---|
| CONICYT |
| Comisión Nacional de Investigación Científica y Tecnológica |
| Comisión Nacional de Investigación CientÃfica y Tecnológica |
| Departamento de IngenierÃa Mecánica, Universidad de Chile |
| Departamento de Postgrado y Postitulo, Universidad de Chile |
| Chilean government through the Comision Nacional de Ciencia y Tecnologia-CONICYT (Anillo ACT-18) |
| Comisio¤ n Nacional de Ciencia y Tecnolog |
| Departamento de Postgrado y Post|¤tulo, Universidad de Chile |
| Agradecimiento |
|---|
| This work was supported by the Chilean government through the Comision Nacional de Ciencia y Tecnologia-CONICYT (Anillo ACT-18 project, PBCT program). Additional funding was provided by the Departamento de Postgrado y Postitulo, Universidad de Chile. This work is part of the PhD thesis of M. Munoz, which was supported by a 4 years grant from CONICYT. |
| This work was supported by the Chilean government through the Comisio¤ n Nacional de Ciencia y Tecnolog|¤a^ CONICYT (Anillo ACT-18 project, PBCT program). Additional funding was provided by the Departamento de Postgrado y Post|¤tulo, Universidad de Chile. This work is part of the PhD thesis of M. Mun‹ oz, which was supported by a 4 years grant from CONICYT. |
