Flotation of Magnetite Crystals upon Decompression - A Formation Model for Kiruna-type Iron Oxide-Apatite Deposits
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
Bibliographic Details
Main Authors: |
Knipping, Jaayke L,
Simon, Adam C,
Fiege, A,
Webster, J D,
Reich, Martín,
Barra-Pantoja, Luis Fernando,
Holtz F,
Oeser-Rabe, M |
Language: | English |
Subjects: |
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Online Access: | http://hdl.handle.net/10533/233203
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