| dc.date.accessioned | 2020-03-11T20:26:50Z | |
| dc.date.accessioned | 2022-10-18T22:41:40Z | |
| dc.date.available | 2020-03-11T20:26:50Z | |
| dc.date.available | 2022-10-18T22:41:40Z | |
| dc.date.created | 2020-03-11T20:26:50Z | |
| dc.date.issued | 2015 | |
| dc.identifier | http://hdl.handle.net/10533/238118 | |
| dc.identifier | 15090013 | |
| dc.identifier | WOS:000359013400009 | |
| dc.identifier | no scielo | |
| dc.identifier | eid=2-s2.0-84934760862 | |
| dc.identifier.uri | https://repositorioslatinoamericanos.uchile.cl/handle/2250/4469457 | |
| dc.description.abstract | Kiruna-type iron oxide–apatite (IOA) deposits are an important source of Fe ore, and two radically different processes are being actively investigated for their origin. One hypothesis invokes direct crystallization of immiscible Fe-rich melt that separate | |
| dc.language | eng | |
| dc.relation | https://doi.org/10.1130/G36650.1 | |
| dc.relation | 10.1130/G36650.1 | |
| dc.rights | info:eu-repo/semantics/openAccess | |
| dc.rights | Atribución-NoComercial-SinDerivadas 3.0 Chile | |
| dc.rights | http://creativecommons.org/licenses/by-nc-nd/3.0/cl/ | |
| dc.title | Giant Kiruna-type deposits form by efficient flotation of magmatic magnetite suspensions | |
| dc.type | Articulo | |
