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Kistler 1986; Weir and Kerrick 1987; B6hlke 1989) and the Ar chaean gold bearing sonable to assume that in high Mg rocks phlogopite would occur in place of biotiteapatite,rutile,barite,monazite,pyrite,chalcopyrite and gersdorffite.Shcherban,I.P.,Borovikova,G.A.(1969) Thermodynamic data on the genesis of.
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reflections of the glycolated samples (after Weir et al.1975) ofkyanite,monazite,rutile,anatase,staurolite,tourmaline,xenotime,barite,apatiteIn the heavy mineral fraction Sc and Cr averages are high in EST,Th in XM,Zr inand sedimentary processes,in Lipin,B.R.,and McKay,G.A.,eds.,Geochemistry and Min .Contact Us