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:
Kiruna
Online Access:http://hdl.handle.net/10533/233203
Description
Summary: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

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