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《Journal of Jiling University (Earth Science Edition)》 1988-02
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NEW RECOGNITION OF PANZHIHUA LAYERED ORE BEARING COMPLEX

Yang Tianqi Jiang Xiudao  
The Panzhihua layered V-Ti-Fe bearing gabbro, according to the 334 Ma K-Ar whole rock age up to now has been regarded as to be formed during Hercynian orogeny.This paper, based on detarled field research an age of 1508,5±5.17 Ma of the pyroxene from the pluton by 40Ar/39Ar method, has alloted the pluton to pre-sinian still according to the characteristic sequential evolution in chemical composition and trace elements of the pluton, thecountry rock and the zarrounding basic rocks, the ore bearing gabbro is regarded to be the final evolutionary product of a basic magma; finally, according to the cyclic occurrence of the plutonic body, the formation of the rock and ore is supposed to be multiple episodic and multiple stages.The new recognition provided significant base for investigation and evaluation of the mineral resources in this region.
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10 Su Lianghe Duan Niangao(Beijing Graduate School under Wuhan College of Geology);THE PREDICATION OF LIQUID IMMISCIBILITY IN SILICATE MELTS BY CALCULATING THEIR FREE ENERGIES[J];Geochimica;1989-01
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1 DONG Shuyun, ZHANG Zhaochong State Key Laboratory of Geological Processes and Mineral Resources; China University of Geosciences,Beijing,100083;Geochemical Behavior of Yttrium in Fe—Ti Oxides——An Example Inferred from the Emeishan Large Igneous Province[J];Geological Review;2009-03
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