| 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/10533/233203 | |
| dc.identifier | 1140780 | |
| dc.identifier.uri | https://repositorioslatinoamericanos.uchile.cl/handle/2250/4464560 | |
| dc.description.abstract | Trace-element characteristics of magnetite from Kiruna-type iron oxide-apatite deposits indicate a magmatic origin. A
possible scenario currently considered for the magmatic formation, apart from melt immiscibility, is related to degassing of
volatile-ric | |
| 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 | Flotation of Magnetite Crystals upon Decompression - A Formation Model for Kiruna-type
Iron Oxide-Apatite Deposits | |
| dc.type | Ponencia | |
