Fingerprinting metal transfer from mantle

The ore-forming magmas in post-subduction copper deposits are thought to be derived from the lower crust. The Au-Te fingerprints of post-subduction magmas reveal an important role for the metasomatized sub-crustal lithospheric mantle in the formation of porphyry and epithermal copper deposits.

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Detalles Bibliográficos
Autores principales: Zengqian Hou, Rui Wang
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2019
Materias:
Q
Acceso en línea:https://doaj.org/article/6503184073404d539e68e4ffaed02a2b
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