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Metallization and metallogenetic conditions of Shizhuyuan ultra-large tungsten deposit, Hunan



Metallization and metallogenetic conditions of Shizhuyuan ultra-large tungsten deposit, Hunan



Hunan Dizhi = Hunan Geology 14(4): 211-219



Shizhuyuan ultra-large tungsten deposit formed in the early Yanshanian movement by the activity of magma which is produced from the anatexis of thickened crust in the mantle depression and from the shear-melting of Proterozoic basement. The metallization includes differentiation of crust molten magma, separation of the phases of melt-fluid system and the compositing process of metallization of leaching-distillation- convection of strata materials. With regard to the metallogenetic conditions there are as following: 1) element assemblage very rich in F, Cl and B and magma-hydrothermal solution, that is, the melt-fluid system containing metallogenetic elements; 2) full supply of metallogenetic materials and volatile components with multi-sources; 3) Jurassic water-storing basin providing water source for infiltration and convection, and giving partly the motive power for metallization; 4) the border of two big massifs and the intersections of fault which occur in the heat columns in the zone of magmatic metallization, all these places being favorable tectonic setting for deposit-forming; 5) geochemical field extremely rich in F, W, Sn Mo, Bi, Pb and Zn; 6) high volatile components carrying and transporting metallogenetic materials in very suitable condition of Al and Si media; and 7) the metasomatism and filling and emplacement of metallogenetic materials in upper carbonate rocks.

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