Geochemical characteristics of some rare element-bearing granites in southeast China and physico-chemical conditions of their formation
The formation of ore-bearing granites in the Yenshanian movement in southeast China and the geochemical characteristics of some RE-bearing granites have been studied through multivariate statistical analysis and physicochemical approach. The main conclusions have Been drawn as follows: (1) The granites are believed to be products of anatexis of the crustal materials. The formation temperature of granitic magma is estimated at about 600°C and the crystallization temperatures range from 600° to 500°C. The temperature of Li-, Fand H2O-rich residual magma in the latest stage of magmatism is probably below 500°C. (2) A rock series from early lepidomelane-granite through protolithionite-and zinnwalditegranite to lithioniteor lepidolite-granite is considered as a result of actual crystallization. (3) The mineral paragenesis and fades zonation of granite plutons are mainly controlled by Ph2o, μNa2O and μK2O in the magma. (4) During the magmatic evolution the ore-forming elements (REE, Nb, Ta, etc.) are variable in geochemistry. REEs, similar to mafic components, were highly concentrated at the early stage of the magmatic evolution and deposited under favourable conditions in the zinnwaldite-and protolithionite-granites; Nb and Ta have a preference for felsic and volatile components, thus are mainly concentrated at later stages of the magmatic evolution. Nb ore deposits are formed in the lithionite and lepidolite granites, for Ta is intimately associated with Na2O, Li2O, F and H2O.
KeywordsIntrusive Body Granite Pluton Magmatic Evolution Mineral Paragenesis CIPW Norm
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- Department of Geology, Nanjing University, Granitoid Rocks of Various Periods in South China and Their Relations with Mineralization, 1966, published by the Science and Technology Committee of the People’s Republic of China.Google Scholar
- Institute of Geochemistry, Academia Sinica, Geochemistry of Granitoid Rocks in South China, 1979, Science Press, Beijing.Google Scholar
- Research Group of Mine 414, Geology and Exploration, 2(1973).Google Scholar
- Xu Daoyi et al., Introduction of Mathematical Geology, 1977, Science Press, Beijing.Google Scholar
- Stornier Jr. J. C., Amer. Miner. 60, 7–8(1975).Google Scholar
- Tuttle, O. F. et al., Geol. Soc. Amer. Mem’ 740(1958).Google Scholar
- Yoder, H. S. et al., Bull. Geol. Soc. Mmer., 68, 12(1975), part 2.Google Scholar
- Anfilogov, V. N. et al., Geokhimiya, 1(1973).Google Scholar
- Glyuk, D. S. et al., Geokhimiya, 3(1973).Google Scholar
- Kovalenko, V. I. et al., DAN SSSR, 2(1970), 190.Google Scholar
- Korzinskii, G. S., Physicochemical Conditions of Mineral Paragenesis, 1957, Izd. DAN SSSR.Google Scholar