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《Acta Petrologica Sinica》 2013-12
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Geochronology,geochemistry and mineralogy of ore-bearing and ore-barren intermediate-acid intrusive rocks from the Jiurui ore district,Jiangxi Province and their geological implications

XU YaoMing;JIANG ShaoYong;ZHU ZhiYong;ZHOU Wei;KONG FanBin;SUN MingZhi;XIONG YongGen;State Key Laboratory for Mineral Deposits Research,School of Earth Sciences and Engineering,Nanjing University;State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences;Faculty of Earth Resources and Collaborative Innovation Center for Scarce and Strategic Mineral Resources,China University of Geosciences;Northwestern Jiangxi Geological Team,Bureau of Exploration and Development of Geology and Mineral Researches of Jiangxi Province;  
The major types of copper polymetallic ore deposit in Jiurui ore district include porphyry,skarn and massive sulfide types. Porphyry and skarn types are typical magmatic-hydrothermal deposits,and the massive sulfide deposits of Jiurui area occurred along the strata near the sandstone and dolomite boundary but also located near intrusive rocks,which shows that magmatic- hydrothermal fluids may have also played a crucial role in the mineralization processes. In Jiurui area,petrographic characters of ore- barren intrusive rocks are almost the same as ore-bearing samples,and parameters to identify between ore-bearing and ore-barren intrusive rocks as well as how these parameters affect mineralization are still unknown. In order to solve above problems,a detailed study on geochronology,major elemental geochemistry and mineral chemistry was performed for the ore-bearing and ore-barren quartz diorite-porphyrite and granodiorite porphyry from the Jiurui ore district,Jiangxi Province. Zircon U-Pb dating results demonstrate that extensive magmatism was coeval and intensive in this area,with emplacement ages of 138. 2 ± 1. 8Ma to 148. 0 ± 1. 0Ma for the ore- bearing intrusive rocks,and 139. 0 ± 1. 3Ma to 149. 6 ± 3. 0Ma for the ore-barren intrusive rocks,which are consistent within the error range with each other. The variation ranges of SiO 2 and other 9 major oxides are quite similar between ore-bearing and ore-barren intrusive rocks. The average temperatures of ore-bearing and ore-barren intrusive rocks are 769℃ and 723℃ respectively,which are also not much difference. However,the variation range of the ore-bearing intrusive rocks( 580 ~ 915℃) is obviously greater than the ore-barren ones( 656 ~ 796℃). It is remarkable that the average pressure of ore-barren intrusive rocks( 5. 7kbar) is evidently greater than the ore-bearing samples( 1. 4kbar). Therefore,the ore-bearing intrusive rocks from the Jiurui area should have experienced a more distinctive pressure decreasing process,which is quite important to form magmatic aqueous phase and brittle failure for hydrothermal circulation. However,decreasing pressure process of an intrusive rock is not the sufficient condition for mineralization, but a necessary condition. Based on the data from Jiurui area,the mineralization potential is weak when the pressure of intrusive rock exceeds 4kbar. The f O2 of the ore-bearing intrusive rocks has a wider variation range than the ore-barren samples and half of the data are plotted above the HM buffer line,but the f O2 data of the ore-barren samples are all plotted below the HM buffer line,which means that high f O2( higher than HM buffer line) is beneficial to mineralization in Jiurui ore district.
【Fund】: 科技部973项目(2012CB416706);; “十二五”国家科技支撑计划(2011BAB04B03);; 国家自然科学基金项目(41072055)联合资助
【CateGory Index】: P58
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8 WANG Qiang,ZHAO Zhen-hua,XIONG Xia o-lin,XU Ji-feng (Guangzhou Institute of Geochemistr y,Chinese Academy of Sciences,Guangzhou510640,China);Melting of the underplated basaltic lower crust:Evidence from the Shaxi adakitic sodic quartz diorite-porphyrites,Anhui Province,China[J];Geochimica;2001-04
9 LIU Hong1, QIU Jian sheng1,2, LO Ching hua3, XU Xi sheng1,2, LING Wen li4, WANG De zi1(1. Department of Earth Sciences, Nanjing University, Nanjing 210093, China; 2. State Key Laboratory of Mineral Deposit Research, Nanjing University, Nanjing 21;Petrogenesis of the Mesozoic potash-rich volcanic rocks in the Luzong basin, Anhui Province: Geochemical constraints[J];Geochimica;2002-02
10 ZHOU Weijian1, LIU Lin1, LIU Yonghao2, LU Xuefeng1, CHENG Peng1, CHEN Maobai21. Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710075, China; 2. Shanghai Institute of Applied Physics, Chinese Academy of Sciences, Shanghai 201800, China;Study on the ancient copper-mining and smelting relic site in Ruichang, Jiangxi by using ~(14)C-AMS[J];Geochimica;2004-05
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