Iron Oxide – Apatite, Iron Oxide – Copper – Gold Deposits And Magmas: A Bubbly Connection

dc.date.accessioned2019-03-27T15:55:53Z
dc.date.accessioned2022-10-18T22:03:49Z
dc.date.available2019-03-27T15:55:53Z
dc.date.available2022-10-18T22:03:49Z
dc.date.created2019-03-27T15:55:53Z
dc.date.issued2016
dc.identifierhttp://hdl.handle.net/10533/233195
dc.identifier1140780
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4464552
dc.description.abstractIron oxideapatite (IOA) and iron oxidecoppergold deposits (IOCG) are often spatially and temporally related with one another and with coeval magmatism. However, a genetic model that accounts for observations of natural systems remains elusive, with few ob
dc.languageeng
dc.relationinfo:eu-repo/grantAgreement/Fondecyt/1140780
dc.relationAnnual Meeting Of The Geological Society Of America
dc.rightsinfo:eu-repo/semantics/openAccess
dc.titleIron Oxide – Apatite, Iron Oxide – Copper – Gold Deposits And Magmas: A Bubbly Connection
dc.typePonencia


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