dc.date.accessioned | 2019-03-27T15:55:55Z | |
dc.date.accessioned | 2022-10-18T22:03:54Z | |
dc.date.available | 2019-03-27T15:55:55Z | |
dc.date.available | 2022-10-18T22:03:54Z | |
dc.date.created | 2019-03-27T15:55:55Z | |
dc.date.issued | 2017 | |
dc.identifier | http://hdl.handle.net/10533/233204 | |
dc.identifier | 1140780 | |
dc.identifier.uri | https://repositorioslatinoamericanos.uchile.cl/handle/2250/4464561 | |
dc.description.abstract | Determining the age of mineralization of ore deposits is important for understanding the mechanisms and timing of ore
formation. In many cases, however, conventional dateable mineral phases (e.g., zircon, monazite) are lacking in the ore
mineral assemblag | |
dc.language | eng | |
dc.relation | info:eu-repo/grantAgreement/Fondecyt/1140780 | |
dc.relation | AGU (American Geophysical Union) Fall Meeting | |
dc.rights | info:eu-repo/semantics/openAccess | |
dc.title | ID ICPMS Lu-Hf Geochronology of Apatite from Iron-Oxide Apatite (IOA) Deposits, | |
dc.type | Ponencia | |