Magnetic properties related to hydrothermal alteration processes at the Escondida porphyry copper deposit, northern Chile.

Fluid–rock interaction related to the circulation of hydrothermal fluids can strongly modify the physicochemical properties of wall rocks in porphyry Cu deposits. These processes can also produce compositional and textural changes in ferromagnetic mineral

Detalles Bibliográficos
Autores: Riveros, K., Veloso, E., Campos, E., Menzies, A., Véliz, W.
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2014
País:Chile
Idioma:inglés
OAI Identifier:oai:repositorio.anid.cl:10533/238102
Acceso en línea:https://hdl.handle.net/10533/238102
Access Level:acceso abierto
Descripción
Sumario:Fluid–rock interaction related to the circulation of hydrothermal fluids can strongly modify the physicochemical properties of wall rocks in porphyry Cu deposits. These processes can also produce compositional and textural changes in ferromagnetic mineral