An experimental investigation into the partition of Mo between aqueous fluids and felsic melts: Implications for the genesis of porphyry Mo ore deposits

[Display omitted] •Mo easily distributes into coexisting fluids in peralkaline felsic magma.•The DMo always decreased with increasing A/NK in felsic melts.•Carbon dioxide bearing salinity fluids maybe beneficial for increasing the DMo. Most of the world’s large molybdenum (Mo) deposits are genetical...

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Veröffentlicht in:	Ore geology reviews 2021-07, Vol.134, p.104144, Article 104144
Hauptverfasser:	Jiang, Ziqi, Shang, Linbo, Guo, Haihao, Wang, Xin-song, Chen, Chen, Zhou, Yunhe
Format:	Artikel
Sprache:	eng
Schlagworte:	Earth Sciences Felsic melt Hydrothermal fluid Partition coefficient Porphyry molybdenum deposit Sciences of the Universe
Online-Zugang:	Volltext
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