• Core Journal of China
  • DOAJ
  • Scopus
  • Chinese Scientific and Technical Papers and Citations (CSTPC)
  • Chinese Science Citation Database (CSCD)
Xiang-ke ZHOU, Jian-guo WANG, Yin-chun LIU, Guang-jing LI, Heng-yong LEI, Bing MAO. Fluid Inclusion and Sulfur Isotope Study on the Donggualin Gold Deposit in the Ailaoshan Gold Belt[J]. Rock and Mineral Analysis, 2017, 36(4): 430-439. DOI: 10.15898/j.cnki.11-2131/td.201701060002
Citation: Xiang-ke ZHOU, Jian-guo WANG, Yin-chun LIU, Guang-jing LI, Heng-yong LEI, Bing MAO. Fluid Inclusion and Sulfur Isotope Study on the Donggualin Gold Deposit in the Ailaoshan Gold Belt[J]. Rock and Mineral Analysis, 2017, 36(4): 430-439. DOI: 10.15898/j.cnki.11-2131/td.201701060002

Fluid Inclusion and Sulfur Isotope Study on the Donggualin Gold Deposit in the Ailaoshan Gold Belt

More Information
  • Received Date: January 05, 2017
  • Revised Date: June 06, 2017
  • Accepted Date: June 09, 2017
  • Published Date: March 31, 2017
  • Highlights
    · Ore genesis can be revealed by the study of fluid inclusions and sulfur isotopes in mineral deposit geology.
    · The results of fluid inclusions suggest that the gold ore-forming fluids are characterized by mid-low temperature and low salinity.
    · The metallogenic materials probably come from the mantle-derived materials related to the lamprophyre with minor crustal contamination.
    · The ore formation of Donggualin gold deposit is mainly related to mantle-derived gold-bearing fluid involved in meteoric water and wall rocks.
    Fluid inclusions and sulfur isotopes can reveal the characteristics of ore-forming fluid and the origin of ore-forming materials, which are important indicators for ore genesis. The Donggualin gold deposit is located in the Zhenyuan gold orefield of the Ailaoshan gold belt. Only a few studies have been carried out on this deposit and thus the ore genesis remains unsolved. Microthermometry of fluid inclusion in veins from two mineralization stages and sulfur isotope analyses of pyrite from ores has been studied, in order to unravel the ore genesis. Fluid inclusion results show that the ore-forming fluids belong mainly to the NaCl-H2O system and the homogenization temperatures range from 100℃ to 400℃, with two peak values of 160-190℃ and 280-310℃. The salinities peak at 6%-9% NaCleqv. The densities have two peaks of 0.7-0.8 g/cm3 and 0.9-1.0 g/cm3. These results suggest that the gold-forming fluids are characterized by mid-low temperature and low salinity. The δ34S values of pyrite from the two stages are 0-1‰ and -4.7‰-3‰, respectively, which are generally consistent with those of the lamprophyre wallrock (-0.44‰-0.54‰). The lamprophyre is very close to gold mineralization and lamprophyre-hosted ore is the most common. It can be inferred that the ore materials are probably related to the lamprophyre derived from mantle related to minor crustal contamination. In conclusion, the Donggualin deposit was possibly formed by mantle-derived gold-bearing fluids involved in meteoric water and wall rocks. This research provides an important clue for the ore genesis of the Donggualin gold deposit and gold deposits in the Ailaoshan gold belt.
  • 陈永清, 黄静宁, 卢映祥, 等.中缅毗邻区金腊Pb-Zn-Ag多金属矿田元素、稳定同位素和流体包裹体地球化学[J].地球科学——中国地质大学学报, 2009, 34(4):585-594. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200904004.htm

    Chen Y Q, Huang J N, Lu Y X, et al.Geochemistry of elements, sulphur-lead isotopes and fluid inclusions from Jinla Pb-Zn-Ag poly-metallic ore field at the joint area across China and Myanmar border[J].Earth Science-Journal of China University of Geosciences, 2009, 34(4):585-594. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200904004.htm
    付伟, 柴明春, 杨启军, 等.广西佛子冲大型铅锌多金属矿床的成因:流体包裹体和H-O-S-Pb同位素地球化学约束[J].岩石学报, 2013, 29(12):4136-4150. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201312007.htm

    Fu W, Chai M C, Yang Q J, et al.Genesis of the Fozichong Pb-Zn polymetallic deposit:Constraints from fluid inclusions and H-O-S-Pb isotopic evidences[J].Acta Petrologica Sinica, 2013, 29(12):4136-4150. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201312007.htm
    倪培, 范宏瑞, 丁俊英.流体包裹体研究进展[J].矿物岩石地球化学通报, 2014, 33(1):1-5. http://www.cnki.com.cn/Article/CJFDTOTAL-KYDH201401001.htm

    Ni P, Fan H R, Ding J Y.Progress in fluid inclusions[J].Bulletin of Mineralogy, Petrology and Geochemistry, 2014, 33(1):1-5. http://www.cnki.com.cn/Article/CJFDTOTAL-KYDH201401001.htm
    孙晓明, 莫儒伟, 翟伟, 等.藏南沙拉岗锑矿流体包裹体红外显微测温研究[J].岩石学报, 2014, 30(1):189-198. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201401014.htm

    Sun X M, Mo R W, Zhai W, et al.Infrared fluid inclusion microthemometry on stibnite from Shalagang antimony ore in Southern Tibet, China[J].Acta Petrologica Sinica, 2014, 30(1):189-198. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201401014.htm
    张潮, 刘育, 刘向东, 等.胶西北新城金矿床硫同位素地球化学[J].岩石学报, 2014, 30(9):2495-2506. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201409004.htm

    Zhang C, Liu Y, Liu X D, et al.Characteristics of sulfur isotope geochemistry of the Xincheng gold deposit, Northwest Jiaodong, China[J].Acta Petrologica Sinica, 2014, 30(9):2495-2506. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201409004.htm
    贾丽琼, 徐文艺, 杨丹, 等.江西九瑞地区东雷湾矽卡岩型铜多金属矿床流体包裹体特征及稳定同位素地球化学研究[J].岩石矿物学杂志, 2015, 34(2):184-204. http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW201502005.htm

    Jia L Q, Xu W Y, Yang D, et al.Fluid inclusion characteristics and stable isotope geochemistry of the Dongleiwan skarn Cu polymetallic deposit in the Jiujiang-Ruichang metallogenic area, Jiangxi Province[J].Acta Petrologica et Mineralogica, 2015, 34(2):184-204. http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW201502005.htm
    卢焕章, 单强.金属矿床的成矿流体成分和流体包裹体[J].岩石学报, 2015, 31(4):1108-1116. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201504018.htm

    Lu H Z, Shan Q.Composition of ore forming fluids in metal deposits and fluid inclusion[J].Acta Petrologica Sinica, 2015, 31(4):1108-1116. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201504018.htm
    王洋洋, 肖益林, 杨晓勇.长江中下游成矿带铜陵新桥矿床Re-Os同位素及流体包裹体研究[J].岩石学报, 2015, 31(4):1031-1039. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201504011.htm

    Wang Y Y, Xiao Y L, Yang X Y.Re-Os isotope systematics and fluid inclusions of Xinqiao deposit in Tongling, the middle-lower Yangtze River metallogenic belt[J].Acta Petrologica Sinica, 2015, 31(4):1031-1039. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201504011.htm
    赵静, 梁金龙, 倪师军, 等.甘肃阳山金矿载金黄铁矿硫同位素Nano-SIMS原位分析[J].矿床地质, 2016, 35(4):653-662. http://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ201604002.htm

    Zhao J, Liang J L, Ni S J, et al.In situ sulfur isotopic composition analysis of Au-bearing pyrites by using nano-SIMS in Yangshan gold deposit, Gansu Province[J].Mineral Deposit, 2016, 35(4):653-662. http://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ201604002.htm
    丁矢勇.论老王寨金矿田(段)地球化学特征[J].云南地质, 1995, 14(3):206-215. http://www.cnki.com.cn/Article/CJFDTOTAL-YNZD503.003.htm

    Ding S Y.Discussion on the geochemical characteristics of Laowangzhai gold ore field[J].Yunnan Geology, 1995, 14(3):206-215. http://www.cnki.com.cn/Article/CJFDTOTAL-YNZD503.003.htm
    张闯, 杨立强, 赵凯, 等.滇西哀牢山老王寨金矿床控矿构造样式[J].岩石学报, 2012, 28(12):4109-4124. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201212024.htm

    Zhang C, Yang L Q, Zhao K, et al.Structure controlling pattern of the Laowangzhai gold deposit, Ailaoshan orogenic belt, Western Yunnan, China[J].Acta Petrologica Sinica, 2012, 28(12):4109-4124. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201212024.htm
    黄智龙, 刘从强, 朱成明, 等.云南老王寨金矿区煌斑岩成因及其与金矿化的关系[M].北京:地质出版社, 1999:1-252.

    Huang Z L, Liu C Q, Zhu C M, et al.The Origin of Lamprophyres in the Laowangzhai Gold Field, Yunnan Province and Their Relations with Gold Mineralization[M].Beijing:Geological Publishing House, 1999:1-252.
    梁业恒, 孙晓明, 石贵勇, 等.云南哀牢山老王寨大型造山型金矿成矿流体地球化学[J].岩石学报, 2011, 27(9):2533-2540. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201109005.htm

    Liang Y H, Sun X M, Shi G Y, et al.Ore-forming fluid geochemistry and genesis of Laowangzhai large scale orogenic gold deposit in Ailaoshan gold belt, Yunnan Province, China[J].Acta Petrologica Sinica, 2011, 27(9):2533-2540. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201109005.htm
    Zhao Y, Wang Q F, Sun X, et al.Characteristics of ore-forming fluid in the Zhenyuan gold orefield, Yunnan Province, China[J].Journal of Earth Science, 2013, 24(2):203-211. doi: 10.1007/s12583-013-0323-4
    何文举.镇沅金矿田围岩蚀变与成矿系列[J].云南地质, 2002, 21(2):121-133. http://www.cnki.com.cn/Article/CJFDTOTAL-YNZD200202001.htm

    He W J.Wallrock alteration and metallongenic series of Zhenyuan Au ore field[J].Yunnan Geology, 2002, 21(2):121-133. http://www.cnki.com.cn/Article/CJFDTOTAL-YNZD200202001.htm
    沈上越, 魏启荣, 程惠兰, 等.云南哀牢山金矿带成因类型探讨[J].特提斯地质, 1997(21):73-84. http://www.cnki.com.cn/Article/CJFDTOTAL-TTSD721.005.htm

    Shen S Y, Wei Q R, Cheng H L, et al.An approach to genetic types of the gold deposits in the Ailaoshan gold ore belt, Yunnan[J].Tethyan Geology, 1997(21):73-84. http://www.cnki.com.cn/Article/CJFDTOTAL-TTSD721.005.htm
    周向科, 王建国, 易锦俊, 等.云南冬瓜林金矿床的围岩蚀变特征和成矿阶段划分[J].中国矿业, 2016, 25(增刊):285-288. http://www.cnki.com.cn/Article/CJFDTOTAL-ZGKA2016S1072.htm

    Zhou X K, Wang J G, Yi J J, et al.Wall rock alteration and ore-forming hydrothermal process division of Donggualin gold deposit, Yunnan[J].China Mining Magazine, 2016, 25(Supplement):285-288. http://www.cnki.com.cn/Article/CJFDTOTAL-ZGKA2016S1072.htm
    侯增谦, 吕庆田, 王安建, 等.初论陆-陆碰撞与成矿作用——以青藏高原造山带为例[J].矿床地质, 2003, 22(4):319-333. http://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ200304000.htm

    Hou Z Q, Lü Q T, Wang A J, et al.Continental collision and related metallogeny:A case study of mineralization in Tibetan orogen[J].Mineral Deposits, 2003, 22(4):319-333. http://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ200304000.htm
    杨立强, 邓军, 赵凯, 等.哀牢山造山带金矿成矿时序及其动力学背景探讨[J].岩石学报, 2011, 27(9):2519-2532. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201109004.htm

    Yang L Q, Deng J, Zhao K, et al.Tectono-thermochronology and gold mineralization events of orogenic gold deposits in Ailaoshan orogenic belt, Southwest China:Geochronological constraints[J].Acta Petrologica Sinica, 2011, 27(9):2519-2532. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201109004.htm
    吴海威, 张连生, 嵇少丞.红河-哀牢山断裂带喜山期陆内大型左行走滑剪切带[J].地质科学, 1989, 10(1):1-8. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX198901000.htm

    Wu H W, Zhang L S, Ji S C.The Red River-Ailaoshan Fault zone-A Himalayan large sinistral strike slip intracontinental shear zone[J].Chinese Journal of Geology, 1989, 10(1):1-8. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX198901000.htm
    胡云中, 唐尚鹑, 王海平, 等.哀牢山金矿地质[M].北京:地质出版社, 1995:1-278.

    Hu Y Z, Tang S C, Wang H P, et al.Geology of Gold Deposits in Ailaoshan[M].Beijing:Geological Publishing House, 1995:1-278.
    胡瑞忠, 毕献武, 何明友, 等.哀牢山金矿带矿化剂对金成矿的制约[J].中国科学(D辑), 1998, 28(增刊):24-30. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK1998S2003.htm

    Hu R Z, Bi X W, He M Y, et al.Constrains from mineralizing agent to gold mineralization in the Ailaoshan gold metallogenic belt[J].Science in China (Series D), 1998, 28(Supplement):24-30. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK1998S2003.htm
    赵岩, 黄钰涵, 梁坤, 等.西南三江地区镇沅金矿载金黄铁矿稀土与微量元素特征[J].岩石学报, 2015, 31(11):3297-3308. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201511010.htm

    Zhao Y, Huang Y H, Liang K, et al.Rare earth element and trace element features of auriferous pyrite in the Zhenyuan gold deposit, Sanjiang region, Yunnan Province, China[J].Acta Petrologica Sinica, 2015, 31(11):3297-3308. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201511010.htm
    何文举.镇沅金矿田煌斑岩特征及其与金矿成矿的关系[J].云南地质, 1993, 12(2):148-158. http://www.cnki.com.cn/Article/CJFDTOTAL-YNZD199302001.htm

    He W J.Characteristics of the lamprophyre and the relation with gold mineralization in Zhenyuan gold mine field[J].Yunnan Geology, 1993, 12(2):148-158. http://www.cnki.com.cn/Article/CJFDTOTAL-YNZD199302001.htm
    李定谋, 曹志敏, 覃功炯, 等.哀牢山蛇绿混杂岩带金矿床[M].北京:地质出版社, 1998:1-137.

    Li D M, Cao Z M, Tan G J, et al.Gold Deposits in Ailaoshan Ophiolitic Melange Zone[M].Beijing:Geological Publishing House, 1998:1-137.
    侯增谦.大陆碰撞成矿论[J].地质学报, 2010, 84(1):30-58. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201001001.htm

    Hou Z Q.Metallogensis of continental collision[J].Acta Geologica Sinica, 2010, 84(1):30-58. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201001001.htm
    杨立强, 刘江涛, 张闯, 等.哀牢山造山型金成矿系统:复合造山构造演化与成矿作用初探[J].岩石学报, 2010, 26(6):1723-1739. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201006008.htm

    Yang L Q, Liu J T, Zhang C, et al.Superimposed orogenesis and metallogenesis:An example from the orogenic gold deposits in Ailaoshan gold belt, Southwest China[J].Acta Petrologica Sinica, 2010, 26(6):1723-1739. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201006008.htm
    黄智龙.幔源岩浆活动过程中的去气作用——以云南老王寨金矿煌斑岩为例[J].矿物岩石地球化学通报, 2001, 20(1):l-5. http://www.cnki.com.cn/Article/CJFDTOTAL-KYDH200101001.htm

    Huang Z L.Degassing in the processes of mantle-derived magmatism:As exemplified by lamprophyres in Laowangzhai gold deposit, Yunnan Province[J].Bulletin of Mineralogy, Petrology and Geochemistry, 2001, 20(1):l-5. http://www.cnki.com.cn/Article/CJFDTOTAL-KYDH200101001.htm
    卢焕章, 范宏瑞, 倪培, 等.流体包裹体[M].北京:科学出版社, 2004:1-487.

    Lu H Z, Fan H R, Ni P, et al.Fluid Inclusions[M].Beijing:Science Press, 2004:1-487.
    王志海, 叶美芳, 董会, 等.流体包裹体盐度低温拉曼光谱测定方法研究[J].岩矿测试, 2014, 33(6):813-821. http://www.ykcs.ac.cn/ykcs/ch/reader/view_abstract.aspx?file_no=20140609&flag=1

    Wang Z H, Ye M F, Dong H, et al.Study on salinity determination of fluid inclusions by cryogenic Raman spectroscopy[J].Rock and Mineral Analysis, 2014, 33(6):813-821. http://www.ykcs.ac.cn/ykcs/ch/reader/view_abstract.aspx?file_no=20140609&flag=1
    Bodnar R J.Reviced equation and table for determining the freezing point depression of H2O-NaCl solutions[J].Geochimica et Cosmomochim Acta, 1993, 57:683-684. doi: 10.1016/0016-7037(93)90378-A
    刘斌, 沈昆.流体包裹体热力学[M].北京:地质出版社, 1999:1-290.

    Liu B, Shen K.Fluid Inclusion Thermodynamics[M].Beijing:Geological Publishing House, 1999:1-290.
    刘江涛, 杨立强, 吕亮.中甸普朗还原性斑岩型铜矿床:矿物组合与流体组成约束[J].岩石学报, 2013, 29(11):3914-3924. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201311022.htm

    Liu J T, Yang L Q, Lü L.Pulang reduced porphyry copper deposit in the Zhongdian area, Northwest China:Constrains by the mineral assemblages and the ore-forming fluid compositions[J].Acta Petrologica Sinica, 2013, 29(11):3914-3924. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201311022.htm
    张静, 杨艳, 胡海珠, 等.河南银洞沟造山型银矿床碳硫铅同位素地球化学[J].岩石学报, 2009, 25(11):2833-2842. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200911015.htm

    Zhang J, Yang Y, Hu H Z, et al.C-S-Pb isotope geochemistry of the Yindonggou orogenic type silver deposit in Henan Province[J].Acta Petrologica Sinica, 2009, 25(11):2833-2842. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200911015.htm
    刘军, 武广, 王峰, 等.黑龙江省岔路口斑岩钼矿床流体包裹体和稳定同位素特征[J].中国地质, 2013, 40(4):1231-1251. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201304022.htm

    Liu J, Wu G, Wang F, et al.Fluid inclusions and stable isotope characteristics of the Chalukou porphyry Mo deposit in Heilongjiang Province[J].Geology in China, 2013, 40(4):1231-1251. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201304022.htm
    郑永飞, 陈江峰.稳定同位素地球化学[M].北京:科学出版社, 2000:1-239.

    Zheng Y F, Chen J F.Stable Isotope Geochemistry[M].Beijing:Science Press, 2000:1-239.
    Rock N M S, Groves D I.Can lamprophyres resolve the genetic controversy over mesothermal gold deposit?[J].Geology, 1988, 16(6):538-541. doi: 10.1130/0091-7613(1988)016<0538:CLRTGC>2.3.CO;2
    任胜利.云南镇沅老王寨-东瓜林金矿床的地球化学研究[J].矿物岩石地球化学通讯, 1993(4):199-201. http://www.cnki.com.cn/Article/CJFDTOTAL-KYDH199304007.htm

    Ren S L.Geochemical study on the Laowangzhai-Donggualin gold deposit in Zhenyuan, Yunnan Province[J].Bulletin of Mineralogy, Petrology and Geochemistry, 1993(4):199-201. http://www.cnki.com.cn/Article/CJFDTOTAL-KYDH199304007.htm
    孙忠实, 邓军, 翟裕生, 等.幔源含金流体主动就位与容矿断裂形成机制[J].地质地球化学, 1999, 27(4):17-22. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDQ199904002.htm

    Sun Z S, Deng J, Zhai Y S, et al.Positive emplacement of mantle gold-bearing fluid and forming mechanism of ore-controlling structures[J].Geology-Geochemistry, 1999, 27(4):17-22. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDQ199904002.htm
    边千韬.地球壳幔结构构造与老王寨超大型金矿床形成关系探索[J].中国科学(D辑), 1998, 28(4):303-309. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK199804002.htm

    Bian Q T.Preliminary study on the relationship between the crust-mantle structure and the formation of Laowangzhai superlarge gold deposit[J].Science in China (Series D), 1998, 28(4):303-309. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK199804002.htm
    李光勋. 云南哀牢山老王寨金矿矿田构造分析[C]//青藏高原地质文集. 1990: 187-197.

    Li G X.Structural Analysis of the Laowangzhai Gold Orefield, Ailaoshan Mountain[C]//Proceedings of the Geology of the Qingha-Xizang (Tibet) Plateau.1990:187-197.
    Yang L Q, Deng J, Goldfarb R J, et al.40Ar/39Ar geochronological constraints on the formation of the Dayingezhuang gold deposit:New implications for timing and duration of hydrothermal activity in the Jiaodong gold province, China[J].Gondwana Research, 2014, 25(4):1469-1483. doi: 10.1016/j.gr.2013.07.001
    侯增谦, 潘桂棠, 王安建, 等.青藏高原碰撞造山带:Ⅱ.晚碰撞转换成矿作用[J].矿床地质, 2006, 25(5):521-543. http://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ200605000.htm

    Hou Z Q, Pan G T, Wang A J, et al.Metallogenesis in Tibetan collisional orogenic belt:Ⅱ.Mineralization in late collisional transformation setting[J].Mineral Deposits, 2006, 25(5):521-543. http://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ200605000.htm
    侯增谦, 莫宣学, 杨志明, 等.青藏高原碰撞造山带成矿作用:构造背景、时空分布和主要类型[J].中国地质, 2006, 33(2):340-351. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200602013.htm

    Hou Z Q, Mo X X, Yang Z M, et al.Metallogeneses in the collisional orogen of the Qinghai-Tibet plateau:Tectonic setting, tempo-spatial distribution and ore deposit types[J].Geology in China, 2006, 33(2):340-351. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200602013.htm

Catalog

    Article views (2442) PDF downloads (45) Cited by()

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return