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《Geotectonica et Metallogenia》 2014-02
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Metallogenetic Specialization of the Fluorite-bearing Granites in the Northern Part of the Eastern Nanling Region

FANG Guicong;WANG Denghong;CHEN Zhenyu;CHEN Zhenghui;ZHAO Zheng;GUO Naxin;College of Earth Science, Guilin University of Technology;Chinese Academy of Geological Sciences;MLR Key Laboratory of Metallogeny and Mineral Resources Assessment,Institute of Mineral Resources, Chinese Academy of Geological Sciences;  
Fluorite deposits in the northern part of the eastern Nanling region are intimately associated with granitic intrusions. To investigate their fluorite-metallogenetic specialization, the chemical compositions of biotites and whole rock of the granites were analyzed. The granites are divided into two groups: fluorite-bearing and fluorite-barren granites. The fluorite-bearing granites are mainly biotite granites, high potassium calc-alkaline, whose accessory minerals commonly include fluorite. The fluorite-bearing granites have higher Mo contents and lower Th/U ratios than those of the fluorite-barren counterparts. Biotite in the fluorite-bearing granites is ferruginous biotite and siderophyllite biotite, which are characterized by higher contents of TiO2, MgO, Cl, and F and lower contents of Al2O3, TFe2O3 than those of the fluorite-barren granites. F and Cl contents of the fluorite-bearing granites show an obvious positive correlation, while the F and Al2O3 contents negatively correlated. The compositions of the biotites indicate that the fluorite-bearing granites were mainly derived from crustal sources with involvement of the mantle, and crystallized at conditions of high temperature, low pressure and high fO2.
【Fund】: 国家深部探测技术与实验研究专项“南岭成矿带地壳岩浆系统结构探测实验”(编号:SinoProbe-03-01);; 中国地质大调查项目“南岭地区岩浆岩成矿专属性研究”(编号:1212011120989)、中国地质大调查项目“广东诸广山南部整装勘查区铀多金属矿成矿地质条件与综合找矿方法研究”(编号:12120113090500)资助;; 国土资源部成矿作用与资源评价重点实验室开放研究项目“南岭科学钻(SP-NLSD-2)花岗岩-云英岩化带-钨矿石英脉:地球化学特征及岩浆-流体演化”、“我国重要矿产和区域成矿规律研究”课题(编号:1212010633903)、“南岭于都-赣县矿集区立体探测技术与深部成矿预测示范”课题(编号:201011048)
【CateGory Index】: P619.215
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