江西朱溪铜钨矿床成因:来自矿物学和年代学的启示

doi:10.13278/j.cnki.jjuese.20170092

吉林大学学报(地球科学版) ›› 2018, Vol. 48 ›› Issue (4): 1050-1070.doi: 10.13278/j.cnki.jjuese.20170092

江西朱溪铜钨矿床成因:来自矿物学和年代学的启示

贺晓龙¹, 张达¹, 陈国华², 狄永军¹, 霍海龙^1,3, 李宁¹, 张志辉^1,4, 饶建锋², 魏锦², 欧阳永棚²

1. 中国地质大学地球科学与资源学院, 北京 100083;
2. 江西省地质矿产勘查开发局912大队, 江西鹰潭 335001;
3. 中国地质科学院地质力学研究所, 北京 100081;
4. 中国地质调查局发展研究中心, 北京 100120

收稿日期:2017-09-25 出版日期:2018-07-26 发布日期:2018-07-26
通讯作者: 张达(1967-),男,教授,博士生导师,主要从事区域构造、区域成矿规律方面的研究,E-mail:zhangda@cugb.edu.cn E-mail:zhangda@cugb.edu.cn
作者简介:贺晓龙(1992-),男,硕士研究生,主要从事矿床成因及成矿动力学方面的研究,E-mail:550453365@qq.com
基金资助:
国土资源部公益性行业科研专项经费（201411035-3）

Genesis of Zhuxi Copper-Tungsten Deposit in Jiangxi Province: Insights from Mineralogy and Chronology

He Xiaolong¹, Zhang Da¹, Chen Guohua², Di Yongjun¹, Huo Hailong^1,3, Li Ning¹, Zhang Zhihui^1,4, Rao Jianfeng², Wei Jin², Ouyang Yongpeng²

1. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China;
2. 912 Geological Team, Bureau of Geology and Mineral Resources of Jiangxi Province, Yingtan 335001, Jiangxi, China;
3. Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China;
4. Research and Development Center, China Geological Survey, Beijing 100120, China

Received:2017-09-25 Online:2018-07-26 Published:2018-07-26
Supported by:
Supported by Public Welfare Foundation for Scientific Researchin the Ministry of Land and Resources(201411035-3)

摘要/Abstract

摘要： 江西景德镇朱溪铜钨矿床是近年来发现的一个世界级超大型铜钨矿床。矿床地质特征、矽卡岩矿物学和成矿岩体年代学的研究表明，矿体赋存于上石炭统黄龙组大理岩与新元古界双桥山群变质岩之间的不整合界面之上，空间上具有明显的矿物组合分带特征。根据矽卡岩产状、矿物共生组合和相互关系，把成矿作用划分为矽卡岩阶段、退化蚀变阶段、石英-硫化物阶段、碳酸盐-萤石阶段。代表性的矽卡岩矿物组合有石榴子石、透辉石、透闪石、硅灰石、符山石、蛇纹石、绿泥石等。电子探针分析表明，石榴子石为钙铝榴石—钙铁榴石系列，辉石为透辉石—钙铁辉石系列。同位素年代学及岩浆与成矿关系的研究表明：花岗闪长岩与早期矽卡岩型矿化相关，矿化范围较小，矿石品位较低；黑云母花岗岩与云英岩型和晚期矽卡岩型的矿化相关，矿化范围较广，矿石品位较高，并获得黑云母花岗岩LA-ICP-MS锆石U-Pb年龄为（147.7±2.2）Ma。综合分析指出，朱溪铜钨矿床为晚侏罗世花岗岩浆有关的热液与晚古生代碳酸盐岩发生多阶段交代作用而形成，成矿作用以矽卡岩型和云英岩型为主。

关键词: 朱溪铜钨矿床, 矿物学, 成矿模式, 电子探针, 锆石U-Pb测年

Abstract: The Zhuxi deposit is located in Jingdezhen in Jiangxi Province, which is a world-class super large copper-tungsten deposit,and its genesis remain debated. The research on the geological characteristics, skarn mineralogy and ore-bearing rock chronology show that the orebodies occur in the unconformity interface between the marble of the Upper Carboniferous Huanglong Group and the metamorphic rocks of the Neoproterozoic Shuangqiaoshan Group, and have significant mineral assemblage zonage with the surrounding rocks. According to the skarn occurrence, mineral association, metasomatic and petrographic characteristics, from early to late the mineralization was divided into skarn stage, retrograde alteration stage, quartz-sulfide stage, and carbonate stage. The representative skarn minerals are garnet, diopside, tremolite, wollastonite, vesuvianite, serpentine, chlorite, etc. The electron microprobe analysis shows that the garnet belongs to grossularite-andradite series, and the pyroxene mainly belongs to diopside-andradite series. The study of isotopic chronology and the relationship between magma and mineralization show that the granodiorite is related to the early skarn-type mineralization, and its scale is smaller and the ore grade is low;the biotite granite is related to the greisen-type and late skarn type mineralization with a wide scale and high ore grade. The result of LA-ICP-MS zircon U-Pb dating of the biotite granite is (147.7±2.2)Ma. The comprehensive analysis shows that the Zhuxi copper-tungsten deposit is formed by the multi-stage metasomatism of the Late Jurassic granitic magma related hydrothermal and Late Paleozoic carbonate rocks, and the mineralization is characterized by skarn-type and greisen-type mainly.

Key words: Zhuxi copper-tungsten deposit, mineralogy, metallogenic mode, electron microprobe, zircon U-Pb dating

中图分类号:

P618

贺晓龙, 张达, 陈国华, 狄永军, 霍海龙, 李宁, 张志辉, 饶建锋, 魏锦, 欧阳永棚. 江西朱溪铜钨矿床成因:来自矿物学和年代学的启示[J]. 吉林大学学报(地球科学版), 2018, 48(4): 1050-1070.

He Xiaolong, Zhang Da, Chen Guohua, Di Yongjun, Huo Hailong, Li Ning, Zhang Zhihui, Rao Jianfeng, Wei Jin, Ouyang Yongpeng. Genesis of Zhuxi Copper-Tungsten Deposit in Jiangxi Province: Insights from Mineralogy and Chronology[J]. Journal of Jilin University(Earth Science Edition), 2018, 48(4): 1050-1070.

参考文献

[1] 翟裕生, 王建平, 彭润民,等. 叠加成矿系统与多成因矿床研究[J]. 地学前缘, 2009, 16(6):282-290. Zhai Yusheng, Wang Jianping, Peng Runmin, et al. Research on Superimposed Metallogenic Systems and Polygenetic Mineral Deposits[J]. Earth Science Frontiers, 2009, 16(6):282-290.
[2] 毛景文, 邵拥军, 谢桂青,等. 长江中下游成矿带铜陵矿集区铜多金属矿床模型[J]. 矿床地质, 2009, 28(2):109-119. Mao Jingwen, Shao Yongjun, Xie Guiqing,et al. Mineral Deposit Model for Porphyry-Skarn Polymetallic Copper Deposits in Tongling Ore Dense District of Middle-Lower Yangtze Valley Metallogenic Belt[J]. Mineral Deposits, 2009, 28(2):109-119.
[3] Karimzadeh S A. Garnetizationas a Ground Preparation Process for Copper Mineralization:Evidence from the Mazraeh Skarn Deposit, Iran[J]. Geologische Rundschau, 2010, 99(2):343-356.
[4] Maher K C. Skarn Alteration and Mineralization at Coroccohuayco, Tintaya District,Peru[J]. Economic Geology, 2010, 105(2):263-283.
[5] Einaudi M T. Skarn Deposits[J]. Economic Geology, 1981, 75:317-391.
[6] Meinert L D. Skarns and Skarn Deposits[J]. Geo-science Canada, 1992, 19(4):145-162.
[7] 赵一鸣,林文蔚,毕承思,等.中国矽卡岩矿床[M]. 北京:地质出版社,2012:164-171. Zhao Yiming, Lin Wenwei, Bi Chengsi, et al. China Skarn Deposits[M].Beijing:Geological Publishing House, 2012:164-171.
[8] 周涛发, 范裕, 袁峰. 长江中下游成矿带成岩成矿作用研究进展[J]. 岩石学报, 2008, 24(8):1665-1678. Zhou Taofa, Fan Yu,Yuan Feng. Advances on Petrogensis and Metallogeny Study of the Mineralization Belt of the Middle and Lower Reaches of the Yangtze River Area[J]. Acta Petrologica Sinica, 2008, 24(8):1665-1678.
[9] 杜杨松, 曹毅, 张智宇, 等.安徽沿江地区中生代原地和异地矽卡岩岩浆-热液成矿作用[J].地质学报, 2011, 85(5):699-711. Du Yangsong, Cao Yi, Zhang Zhiyu, et al. Mesozoic In-Situ and External Skarn Magmatic-Hydrothemal Mineralization in the Anhui Segment of the Lower Yangtze Metallogenic Belt[J]. Acta Geologica Sinica, 2011, 85(5):699-711.
[10] 赵劲松,赵斌,李建威,等. 矽卡岩岩浆对中国北方某些矽卡岩型矿床形成的制约:来自包裹体激光拉曼分析证据[J]. 岩石学报,2015, 31(4):1079-1088. Zhao Jinsong, Zhao Bin, Li Jianwei, et al. Magma Control of Magmatic Skarn to the Formation of Some Deposits of Skarn Type:Evidence from Laser Roman Analyses of Inclusions in Minerals[J]. Acta Petrologica Sinica, 2015, 31(4):1079-1088.
[11] 常印佛,刘湘培,吴言昌.长江中下游铜铁成矿带[M]. 北京:地质出版社,1991:1-379. Chang Yinfo, Liu Xiangpei, Wu Yanchang.Cu-Fe Metallogenic Belt in the Middle and Lower Reaches of Yangtze River[M]. Beijing:Geological Publishing House, 1991:1-379.
[12] Larsen R B. Tungsten Skarn Mineralizations in a Regional Metamorphic Terrain in Northern Norway:A Possible Metamorphic Ore Deposit[J]. Mineralium Deposita, 1991, 26(4):281-289.
[13] 翟裕生,姚书振,林新多,等.长江中下游地区铁铜(金)成矿规律[M].北京:地质出版社,1992:1-235. Zhai Yusheng, Yao Shuzhen, Lin Xinduo, et al. Metallogenic Regularity of Iron-Copper (Gold)in the Middle and Lower Reaches of the Yangtze River[M]. Beijing:Geological Publishing House, 1992:1-235.
[14] 毛景文,李红艳, B Guy,等.湖南柿竹园矽卡岩-云英岩型W-Sn-Mo-Bi矿床地质和成矿作用[J]. 矿床地质, 1996,15(1):1-15. Mao Jingwen, Li Hongyan, Guy B, et al. Geology and Metallogeny of the Shizhuyuan Skarn-Greisen W-Sn-Mo-Bi Deposit, Hunan Province[J]. Mineral Deposits, 1996, 15(1):1-15.
[15] 候增谦,杨竹森,吕庆田,等.安徽铜陵冬瓜山大型铜矿:海底喷流-沉积与矽卡岩化叠加复合成矿过程[J]. 地质学报, 2011,85(5):659-686. Hou Zengqian, Yang Zhusen, Lü Qingtian, et al. The Large-Scale Dongguashan Deposit, Shizishan District in East China:Carboniferous Sedex-Type Massive Sulfides Overprinted by Late Jurassic Skarn Cu Mineralization[J]. Acta Geologica Sinic, 2011, 85(5):659-686.
[16] Meinert L D. Skarns and Skarn Deposits[J]. Geo-science Canada, 1992, 19(4):145-162.
[17] Gaspar L M. Mineralogy and Metasomatic Evolution of Distal Strata-Bound Scheelite Skarns in the Riba de Alva Mine, Northeastern Portugal[J]. Economic Geology, 2000, 95(6):1259-1275.
[18] Mao Jingwen, Xie Guiqing, Duan Chao, et al.A Tectono-Genetic Model for Porphyry-Skarn-Strata Bound Cu-Au-Mo-Fe and Magnetite-Apatite Deposits Along the Middle-Lower Yangtze River Valley,Eastern China[J].Ore Geology Reviews, 2011, 243(1):294-314.
[19] Peng Huijuan, Zhang Chaoqing, Mao Jingwen, et al.Garnets in Porphyry-Skarn Systems:A LA-ICP-MS, Fluid Inclusion, and Stable Isotope Study of Garnets from the Hongniu-Hongshan Copper Deposit, Zhongdian Area, NW Yunnan Province, China[J].Journal of Asian Earth Sciences, 2014, 103:229-251.
[20] Soloviev S G. Geology,Mineralization,and Fluid Inclusion Characteristics of the Kensu W-Mo Skarn and Mo-W-Cu-Au Alkalic Porphyry Deposit,Tien Shan,Kyrgyzstan[J].Economic Geology, 2011,106(2):193-222.
[21] 于淼,丰成友,刘洪川,等. 青海尕林格铁矿床电气石矿物学、元素地球化学及成因研究[J].矿床地质, 2016, 35(1):69-84. Yu Miao, Feng Chengyou, Liu Hongchuan, et al. Mineralogy, Element Geochemistry and Genesis of Tourmaline from Galinge Skarn Deposit, Qinghai Province[J]. Mineral Deposits, 2016, 35(1):69-84.
[22] 丰成友,张德全,项新葵,等.赣西北大湖塘钨矿床辉钼矿Re-Os同位素定年及其意义[J].岩石学报,2012, 28(12):3858-3868. Feng Chengyou, Zhang Dequan, Xiang Xinkui, et al. Re-Os Isotopic Dating of Molybdenite from the Dahutang Tungsten Deposit in Northwestern Jiangxi Province and Its Geological Implication[J]. Acta Petrologica Sinica, 2012,28(12):3858-3868.
[23] 张家菁,梅玉萍,王登红,等.赣北香炉山白钨矿床的同位素年代学研究及其地质意义[J].地质学报,2008, 82(7):927-931. Zhang Jiajing, Mei Yuping, Wang Denghong, et al.Isochronology Study on the Xianglushan Scheelite Deposit in North Jiangxi Province and Its Geological Significance[J]. Acta Geologica Sinica, 2008, 82(7):927-931.
[24] 刘善宝, 刘战庆, 王成辉,等. 赣东北朱溪超大型钨矿床中白钨矿的稀土、微量元素地球化学特征及其Sm-Nd定年[J].地学前缘, 2017,24(5):17-30. Liu Shanbao, Liu Zhanqing, Wang Chenghui, et al.Geochemical Characteristics of REEs and Trace Elementsand Sm-Nd Dating of Scheelite from the Zhuxi Giant Tungsten Deposit in Northeast Jiangxi[J]. Earth Science Frontiers, 2017,24(5):17-30.
[25] 何细荣,陈国华,刘建光,等. 江西景德镇朱溪地区铜钨多金属矿找矿方向[J].中国钨业,2011, 26(1):9-14. He Xirong, Chen Guohua, Liu Jianguang, et al. On the Copper-Tungsten Prospecting Orientation in Zhuxi Region[J]. China Tungsten Industry, 2011, 26(1):9-14.
[26] 陈国华,万浩章,舒良树,等.江西景德镇朱溪铜钨多金属矿床地质特征与控矿条件分析[J].岩石学报,2012, 28(12):3901-3914. Chen Guohua, Wan Haozhang, Shu Liangshu, et al.An Analysis on Ore-Controlling Conditions and Geological Features of the Cu-W Polymetallic Ore Deposit in the Zhuxi Area of Jingdezhen,Jiangxi Province[J]. Acta Petrologica Sinica, 2012, 28(12):3901-3914.
[27] 刘善宝,王成辉,刘战庆,等.赣东北塔前-赋春成矿带岩浆岩时代限定与序列划分及其意义[J].岩矿测试, 2014, 33(4):598-611. Liu Shanbao, Wang Chenghui, Liu Zhanqing, et al.Northeast Jiangxi Taqian-Fuchun Metallogenic Belt Magmatite Time Limit and Sequence Division and Its Significance[J]. Rock and Mineral Analysis, 2014, 33(4):598-611.
[28] 李岩,潘小菲,赵苗,等.景德镇朱溪钨(铜)矿床花岗闪长岩的锆石U-Pb年龄、地球化学特征及其与成矿关系探讨[J].地质论评,2014, 60(3):693-708. Li Yan, Pan Xiaofei, Zhao Miao, et al. LA-ICP-MS Zircon U-Pb Age,Geochemical Features and Relations to the W-Cu Mineralization of Granitic Porphyry in Zhuxi Skarn Deposit,Jingdezhen,Jiangxi[J]. Geological Review, 2014, 60(3):693-708.
[29] 王先广, 刘战庆, 刘善宝,等. 江西朱溪铜钨矿细粒花岗岩LA-ICP-MS锆石U-Pb定年和岩石地球化学研究[J]. 岩矿测试, 2015,34(5):592-599. Wang Xianguang, Liu Zhanqing, Liu Shanbao, et al. LA-ICP-MS Zircon U-Pb Dating and Petrologic Geochemistry of Fine-Grained Granite from Zhuxi Cu-W Deposit, Jiangxi Province and Its Geological Significance[J]. Rock and Mineral Analysis, 2015, 34(5):592-599.
[30] 赵苗,潘小菲,李岩,等.江西朱溪铜钨多金属矿床矽卡岩矿物学特征及其地质意义[J].地质通报,2015, 34(2/3):548-568. Zhao Miao, Pan Xiaofei, Li Yan, et al. Mineralogical Characteristics and Geological Significance of the Zhuxi Cu-W Polymetallic Ore Deposit, Jiangxi Province[J]. Geological Bulletin of China, 2015, 34(2/3):548-568.
[31] 贺晓龙, 张达, 狄永军,等. 江西朱溪铜钨矿床矽卡岩矿物学研究及对成矿过程的启示[J]. 吉林大学学报(地球科学版),2015,45(增刊1):1510. He Xiaolong, Zhang Da, Di Yongjun, et al.Mineralogy of Skarn in the Zhuxi Cu-W Deposit, Jiangxi Province and Its Implication to Mineralization Process[J]. Journal of Jilin University(Earth Science Edition),2015,45(Sup.1):1510.
[32] 徐繁昌,李葆华,王强,等.江西朱溪铜钨多金属矿床流体包裹体研究[J].现代矿业,2016(6):169-170. Xu Fanchang, Li Baohua, Wang Qiang, et al. Fluid Inclusions in Zhuxi Cu-W Polymetallic Deposit, Jiangxi Province[J]. Modern Mining, 2016(6):169-170.
[33] 陈国华,舒良树, 舒立旻,等. 江南东段朱溪钨(铜)多金属矿床的地质特征与成矿背景[J].中国科学:地球科学, 2015,45(12):1799-1818. Chen Guohua, Shu Liangshu, Shu Limin, et al. Geological Characteristics and Mineralization Setting of the Zhuxi Tungsten (Copper) Polymetallic Deposit in the Eastern Jiangnan Orogen[J]. Science China:Earth Sciences, 2015, 45(12):1799-1818.
[34] 霍海龙. 江西景德镇朱溪铜钨矿床控矿构造特征及矿床成因探讨[D].北京:中国地质大学,2016. Huo Hailong.A Preliminary Discussion on Genesis and Structural Control of Zhuxi Copper Tungsten Deposit in Jingdezhen Area of Northeastern Jiangxi Province[D].Beijing:China University of Geosciences, 2016.
[35] 王长明, 吴淦国, 张达,等. 赣东北地区的区域成矿特征和成矿谱系[J]. 世界地质,2010, 29(4):588-600. Wang Changming, Wu Ganguo, Zhang Da, et al. Regional Metallogenic Characteristics and Mineralizing Pedigree in Northeastern Jiangxi[J]. Global Geology, 2010, 29(4):588-600.
[36] Hoskin P W, Black L P. Metamorphic Zircon For-mation by Solid-State Recrystallization of Protolith Igneous Zircon[J]. Journal of Metamorphic Geology, 2000, 18(4):423-439.
[37] Burton J C, Taylor L A. The f_O2-T and f_S2-T Stability Relations of Hedenbergite and of Hedenbergite-Johannsenite Solid Solutions[J]. Economic Geology, 1982, 77(4):764-783.
[38] Meinert L D. Application of Skarn Deposit Zonation Models to Mineral Exploration[J]. Exploration & Mining Geology, 1997, 6(2):185-208.
[39] 赵一鸣,林文蔚,毕承思,等. 中国含金矽卡岩矿床的分布和主要地质特征[J]. 矿床地质,1997,16(3):193-203. Zhao Yiming, Lin Wenwei, Bi Chengsi, et al. The Distribution and Geological Characteristics of Auriferous Skarn Deposits in China[J]. Mineral Deposits, 1997, 16(3):193-203.
[40] 尹京武, 李铉具, 崔庆国,等. 湖南省柿竹园矽卡岩矿床中石榴子石特征[J]. 地球科学:中国地质大学学报, 2000, 25(2):163-171. Yin Jingwu, Li Xuanju, Cui Qingguo, et al. Characteristics of Garnet in Shizhuyuan Skarn Deposit, Hunan Province[J]. Earth Science:Journal of China University of Geosciences, 2000, 25(2):163-171.
[41] 赵一鸣, 张轶男, 林文蔚. 我国矽卡岩矿床中的辉石和似辉石特征及其与金属矿化的关系[J]. 矿床地质, 1997, 16(4):318-319. Zhao Yiming, Zhang Yinan, Lin Wenwei. Characteristics of Pyroxenes and Pyroxenoids in Skarn Deposits of China and Their Relationship with Metallization[J]. Mineral Deposits, 1997, 16(4):318-319.
[42] 邓晋福,赵海玲. 白云母/二云母花岗岩形成与陆内俯冲作用[J].地球科学:中国地质大学学报,1994,19(2):139-147. Deng Jinfu, Zhao Hailing. Generation of Muscovite/Two-Mica Granite and Intracontinental Subduction[J]. Earth Science:Journal of China University of Geosciences,1994,19(2):139-147.
[43] 毛景文,李晓峰,张作衡,等.中国东部中生代浅成热液金矿的类型、特征及其地球动力学背景[J].高校地质学报, 2003, 9(4):620-637. Mao Jingwen, Li Xiaofeng, Zhang Zuoheng, et al. Geology, Distribution, Types and Tectonic Settings of Mesozoic Epithermal Gold Deposits in East China[J]. Geological Journal of China Universities, 2003, 9(4):620-637.
[44] 毛景文, 谢桂青, 李晓峰,等.华南地区中生代大规模成矿作用与岩石圈多阶段伸展[J].地学前缘, 2004, 11(1):45-55. Mao Jingwen, Xie Guiqing, Li Xiaofeng, et al. Mesozoic Large Scale Mineralization and Multiple Lithospheric Extension in South China[J]. Earth Science Frontiers, 2004, 11(1):45-55.
[45] 毛景文,谢桂青,郭春丽,等.南岭地区大规模钨锡多金属成矿作用:成矿时限及地球动力学背景[J].岩石学报,2007, 23(10):2329-2338. Mao Jingwen, Xie Guiqing, Guo Chunli, et al. Large-Scale Tungsten-Tin Mineralization in the Nanling Region, South China:Metallogenic Ages and Corresponding Geodynamic Processes[J]. Acta Petrologica Sinica, 2007, 23(10):2329-2338.
[46] 毛景文,谢桂青,郭春丽,等.华南地区中生代主要金属矿床时空分布规律和成矿环境[J].高校地质学报,2008, 14(4):510-526. Mao Jingwen, Xie Guiqing, Guo Chunli, et al. Spatial-Temporal Distribution of Mesozoic Ore Deposits in South China and Their Metallogenic Settings[J]. Geological Journal of China Universities, 2008, 14(4):510-526.
[47] 毛景文,王志良.中国东部大规模成矿时限及其动力学背景的初步探讨[J].矿床地质, 2000, 19(4):289-296. Mao Jingwen, Wang Zhiliang. A Preliminary Study on Time Limits and Geodynamic Setting of Large-Scale Metallogeny in East China[J]. Mineral Deposits, 2000, 19(4):289-296.
[48] 华仁民,毛景文.试论中国东部中生代成矿大爆发[J].矿床地质,1999, 18(4):300-308. Hua Renmin, Mao Jingwen. A Preliminay Discussion on the Mesozoic Metallogenic Explosion in East China[J]. Mineral Deposits, 1999, 18(4):300-308.
[49] 华仁民,陈培荣,张文兰,等.论华南地区中生代3次大规模成矿作用[J]. 矿床地质,2005, 24(2):99-107. Hua Renmin, Chen Peirong, Zhang Wenlan, et al. Three Majors Metallogenic Events in Mesozoic in South China[J]. Mineral Deposits, 2005, 24(2):99-107.
[50] 毛建仁,邢光福,叶海敏,等.中国东南部及邻区中新生代岩浆作用与成矿[M]. 北京:科学出版社, 2013. Mao Jianren, Xing Guangfu, Ye Haimin, et al.Mesozoic-Cesozoic Magmatic Effect and Metallogenesis in Southeast China and Its Adjacent Regions[M].Beijing:Science Press, 2013.
[51] 王强,赵振华,简平,等.德兴花岗闪长斑岩SHRIMP锆石U-Pb年代学和Nd-Sr同位素地球化学[J].岩石学报,2004, 20(2):315-324. Wang Qiang, Zhao Zhenhua, Jian Ping, et al. SHRIMP Zircon Geochronology and Nd-Sr Isotopic Geochemistry of the Dexing Granodiorite Porphyries[J]. Acta Petrologica Sinica, 2004, 20(2):315-324.
[52] 张志辉,耿林,贾文彬,等.赣北大湖塘钨多金属矿田区域地质特征研究[J].中国矿业,2014(增刊2):133-136. Zhang Zhihui, Geng Lin, Jia Wenbin, et al. Regional Geological Characteristics Study of Tungsten-Polymetallic Ore Field in Dahutang Tungsten Polymetallic Deposit in North of Jiangxi[J]. China Mining Magazine, 2014(Sup.2):133-136.
[53] 黄兰椿,蒋少涌. 江西大湖塘钨矿床似斑状白云母花岗岩锆石U-Pb年代学、地球化学及成因研究[J]. 岩石学报,2012, 28(12):3887-3900. Huang Lanchun, Jiang Shaoyong. Zircon U-Pb Geochronology, Geochemistry and Petrogenesis of the Porphyric-Like Muscovitegranite in the Dahutang Tungsten Deposit,Jiangxi Province[J]. Acta Petrologica Sinica, 2012,28(12):3887-3900.
[54] 黄兰椿, 蒋少涌. 江西大湖塘富钨花岗斑岩年代学、地球化学特征及成因研究[J]. 岩石学报, 2013, 29(12):4323-4335. Huang Lanchun, Jiang Shaoyong. Geochronology, Geochemistry and Petrogenesis of the Tungsten-Bearing Porphyritie Granite in the Dahutang Tungsten Deposit, Jiangxi Province[J]. Acta Petrologica Sinica, 2013, 29(12):4323-4335.
[55] 赵正, 陈毓川, 曾载淋,等. 南岭东段岩前钨矿床地质特征及成岩成矿时代[J]. 吉林大学学报(地球科学版), 2013, 43(6):1828-1839. Zhao Zheng, Chen Yuchuan, Zeng Zailin, et al. Geological Characteristics and Petrogenic & Metallogenic Ages of the Yanqian Tungsten Deposit in Eastern Nanling Region[J]. Journal of Jilin University (Earth Science Edition), 2013, 43(6):1828-1839.
[56] 李晓峰, Yasushi, Watanabe,等. 江西永平铜矿花岗质岩石的岩石结构、地球化学特征及其成矿意义[J]. 岩石学报, 2007, 23(10):2353-2365. Li Xiaofeng, Yasushi, Watanabe, et al. Textures and Geochemical Charactesistics of Granitic Rocks in the Yongping Climax-Type Cu-Mo Deposit, Jiangxi, Southeastern China, and Their Alteration, Mineralization and Tectonic Region[J]. Acta Petrologica Sinica, 2007, 23(10):2353-2365.
[57] 丁昕, 蒋少涌, 倪培,等.江西武山和永平铜矿含矿花岗质岩体锆石SIMS U-Pb年代学[J]. 高校地质学报,2005, 11(3):383-389. Ding Xin, Jiang Shaoyong, Ni Pei, et al. Zircon SIMS U-Pb Geochronology of Host Granitoids in Wushan and Yongping Copper Deposits, Jiangxi Province[J]. Geological Journal of China Universities, 2005, 11(3):383-389.

Metrics

Viewed

Full text

Abstract

Cited

Shared

Discussed

江西朱溪铜钨矿床成因:来自矿物学和年代学的启示

Genesis of Zhuxi Copper-Tungsten Deposit in Jiangxi Province: Insights from Mineralogy and Chronology

PDF (PC)

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

Metrics

本文评价

推荐阅读 10

[1]	蒋川东, 孟璐瑶, 杨麒宇, 王云志, 徐洋, 王言章, 林君. 深部金属矿产地下电磁探测技术进展与展望[J]. 吉林大学学报(地球科学版), 2025, 55(6): 2100-2119.
[2]	张国宾, 冯玥, 赵忠海, 宋学权, 何云龙, 孔金贵. 大兴安岭中段金江沟岩体侏罗纪花岗岩年代学、地球化学特征及其构造意义[J]. 吉林大学学报(地球科学版), 2025, 55(5): 1564-1585.
[3]	颜雪, 王力圆, 陈洲鑫, 张文慧. 福建新生代玄武岩及其地幔包体的矿物学特征——对岩石圈地幔性质的制约 [J]. 吉林大学学报(地球科学版), 2025, 55(2): 463-482.
[4]	王万能, 张耀堂, 李锁明, 吴亮, 袁永盛 . 上扬子西缘晚奥陶世—早志留世重要层位火山活动记录——来自滇东北地区钾质斑脱岩的信息[J]. 吉林大学学报(地球科学版), 2025, 55(1): 155-178.
[5]	刘翔宇, 单玄龙, 衣健, 苏思远, 李嘉慧, 庞赫, 邹玉洁. 渤海湾盆地渤中凹陷义县组火山喷发旋回及其分布规律[J]. 吉林大学学报(地球科学版), 2024, 54(6): 1829-1845.
[6]	吴兆徽, 刘显太, 杜玉山, 吴颖昊. 碳酸盐岩微观测试技术对比与应用——以济阳坳陷乐安油田潜山为例[J]. 吉林大学学报(地球科学版), 2024, 54(5): 1519-1529.
[7]	张坤, 史冬岩, 常翔鲲, 朴星海, 王伟东. 伸展背景下的埃达克质岩：黑龙江呼玛地区早白垩世侵入岩的年代学和地球化学特征[J]. 吉林大学学报(地球科学版), 2024, 54(4): 1248-1263.
[8]	苑东洋, 石威, 刘德民, 黄天统, 徐龙生, 陈超, 孔令耀. 鄂北耿集-板桥地区新元古代变火山岩系地层归属——来自锆石U-Pb测年、Hf同位素的证据 [J]. 吉林大学学报(地球科学版), 2024, 54(2): 516-530.
[9]	徐智涛, 李萌萌, 孙景贵, 孙立影, 冯靖乔, 梁小龙. 大兴安岭得耳布尔地区中侏罗世流纹岩成因及成岩地球动力学背景[J]. 吉林大学学报(地球科学版), 2023, 53(3): 866-886.
[10]	王振亮, 赵克强, 杨剑洲, 邓友茂, 付燕刚, 段壮, 林鲁军, 左光明. 内蒙古架子山地区晚石炭世二长花岗岩成因及其地质意义[J]. 吉林大学学报(地球科学版), 2023, 53(3): 984-1000.
[11]	吴燕清, 王常东, 余弘龙, 周舰, 林天发, 于兵, 董小宇. 内蒙古五十家子—新城子地区火山岩型铀矿地质特征及找矿方向[J]. 吉林大学学报(地球科学版), 2023, 53(2): 418-.
[12]	邰文星, 周琦, 杨成富, 何金坪, 刘光富, 王泽鹏, 赵平 . 黔西南簸箕田金矿床皂矾山构造角砾岩特征及成矿意义 [J]. 吉林大学学报(地球科学版), 2023, 53(1): 106-119.
[13]	许庆林, 孙丰月, 李碧乐, 杨延乾. 青海东昆仑哈陇休玛钼多金属矿床成矿流体特征及成矿模式[J]. 吉林大学学报(地球科学版), 2022, 52(5): 1512-1524.
[14]	张博文, 苏春媚, 冯汉清, 任文林. 西昆仑甜水海黄羊沟闪长玢岩年代学、地球化学特征及构造背景[J]. 吉林大学学报(地球科学版), 2022, 52(5): 1575-1593.
[15]	辛未, 孟元库, 许志河, 孙丰月, 钱烨. 哀牢山成矿带长安金矿床成因：地质特征、流体包裹体测温和H-O-S-Pb同位素制约[J]. 吉林大学学报(地球科学版), 2022, 52(5): 1610-1625.