The formation of phosphorus-iron oxide (P-Fe) immiscible melts and their possible connection to the genesis of Kiruna-type and Nelsonite deposits was experimentally investigated by adding phosphoric acid (H3PO4), water, and sulfur, to andesite at 100-450 MPa, 500-900 degrees C, at the NiNiO and m...
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http://repositoriodigital.uct.cl/handle/10925/3252
Lledo, Haroldo L.
,
Naslund, H. Richard
,
Jenkins, David M.
,
[Experiments on phosphate-silicate liquid immiscibility with potential links to iron oxide apatite and nelsonite deposits]
,
Experiments on phosphate-silicate liquid immiscibility with potential links to iron oxide apatite and nelsonite deposits
