Article ; Online: Immiscible hydrous Fe-Ca-P melt and the origin of iron oxide-apatite ore deposits.
2018 Volume 9, Issue 1, Page(s) 1415
Abstract: ... separation of an iron-rich melt has been invoked, but Fe-Ca-P-rich and Si-poor melts similar in composition ...
Abstract | The origin of iron oxide-apatite deposits is controversial. Silicate liquid immiscibility and separation of an iron-rich melt has been invoked, but Fe-Ca-P-rich and Si-poor melts similar in composition to the ore have never been observed in natural or synthetic magmatic systems. Here we report experiments on intermediate magmas that develop liquid immiscibility at 100 MPa, 1000-1040 °C, and oxygen fugacity conditions (fO |
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Language | English |
Publishing date | 2018-04-12 |
Publishing country | England |
Document type | Journal Article ; Research Support, Non-U.S. Gov't |
ZDB-ID | 2553671-0 |
ISSN | 2041-1723 ; 2041-1723 |
ISSN (online) | 2041-1723 |
ISSN | 2041-1723 |
DOI | 10.1038/s41467-018-03761-4 |
Database | MEDical Literature Analysis and Retrieval System OnLINE |
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