Dissecting the Re-Os molybdenite geochronometer

Rhenium and osmium isotopes have been used for decades to date the formation of molybdenite (MoS2), a common mineral in ore deposits and the world’s main source of molybdenum and rhenium. Understanding the distribution of parent 187Re and radiogenic daugh

Detalles Bibliográficos
Autores: Barra, F., Deditius, A., Reich, M., Kilburn, M.R., Guagliardo, P., Roberts, M.P.
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2017
País:Chile
Idioma:inglés
OAI Identifier:oai:repositorio.anid.cl:10533/238230
Acceso en línea:https://hdl.handle.net/10533/238230
Access Level:acceso abierto
Descripción
Sumario:Rhenium and osmium isotopes have been used for decades to date the formation of molybdenite (MoS2), a common mineral in ore deposits and the world’s main source of molybdenum and rhenium. Understanding the distribution of parent 187Re and radiogenic daugh