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《Geotectonica Et Metallogenia》 2004-03
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GEOCHEMICAL CHARACTERISTICS OF GRANITES AND ITS STRUCTURAL GENETIC ENVIRONMENT IN THE NANDAN-HECHI METALLOGENETIC BELT, NORTHWEST GUANGXI

CAI Minghai~(1,2),LIANG Ting~3,WU Decheng~2 and HUANG Huimin~2 (1.Yichang Institute of Geology and Minerals,Yichang, HB 443003,China; 2.Liuzhou Huaxi Co. Ltd.,Liuzhou, GX 545006,China; 3. School of Earth Sciences and Resources Management, Chang'an University, Xi'an, SX 710054, China)  
The Nandan-Hechi metallogenetic belt is the most important tin-polymetallic producing district in China, and is the location of the Dachang super-large tin deposit. Based on the detailed field investigation and isotopic data, the stages of magmatic activity in the Nandan-Hechi metallogenetic belt have been lined out in this paper. Through the study about the geochemical characteristics of different granites, and by using Al_2O_3 vs SiO_2?TFeO/(TFeO+ MgO) vs SiO_2, AFM, ACF and Rb vs Y+Ta, Rb vs Y+Nb, Ta vs Yb, Nb vs Y discrimination diagrams in combination with regional geological setting analysis, the authors carried out analyses about the structural environment for the formation of the granites, and discussed the structural environment and dynamic setting for the large scale mineralization in this area. Our study indicates that the majority of the granites in Nandan-Hechi metallogenetic belt belong to POG, while the later stage alaskite belongs to RRG+CEUG. The granites were formed at the stage of structure transformation from postorogenic phase to intraplate setting. But the major structural environment is steady regional extension. The formation age for the granites represents the time of this transformation, and this translation environment is favored for large-scale metallogenesis.
【Fund】: 华锡集团有限责任公司博士后工作站科研项目“丹池成矿带构造控矿规律研究”资助
【CateGory Index】: P588.1
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