Fluid inclusion and stable isotope evidence for the genesis of quartz-scheelite veins, Metaggitsi area, central Chalkidiki Peninsula, N. Greece

Scheelite mineralization accompanied by muscovite and albite, and traces of Mo-stolzite and stolzite occurs in epigenetic quartz vein systems hosted by two-mica gneissic schists, and locally amphibolites, of the Paleozoic or older Vertiskos Formation, in the Metaggitsi area, central Chalkidiki, N Gr...

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Veröffentlicht in:	Mineralium deposita 1997-10, Vol.32 (6), p.581-595
Hauptverfasser:	Kilias, S. P., Konnerup-Madsen, J.
Format:	Artikel
Sprache:	eng
Schlagworte:	Fluids Fractionation Geochemistry Homogenization Immiscibility Isotopes Mineralization Mineralogy Paleozoic Quartz Sodium chloride Stable isotopes Veins (geology)
Online-Zugang:	Volltext
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