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《Geochimica》 1998-01
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THE TRACKING STUDY OF Nb AND Ta IN MAGMATICEVOLUTIONARY PROCESS FOR PEGMATITEVEIN No.3, ALTAY, CHINA

Wang Xianjue; Niu Hecai; Guo Guozhang(Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640)  
The fractionation and evolution of some incompatible elements in pegmatite veinNo.3 are studied. The results show that the incompatibility of Nb and Ta is stronglylowered in the evolutionary process of granitic pegmatite magma. The Nb-Ta-independent minerals such as columbite, microlite etc. can form in each evolutionarystage of pegmatitic melts. The fractional crystallization process of pegmatite vein No.3can be reconstructed on the basis of geological observation and laboratory data.Meanwhile, the partition coefficients of Nb and Ta between melts andpegmatite-forming minerals such as muscovite, microcline, albite, spodumene etc. arecalculated in vein No.3 and mineralizations of both Nb and Ta are discussed too.
【Fund】: 国家自然科学基金!49333030
【CateGory Index】: P595
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