吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (5): 1354-1367.doi: 10.13278/j.cnki.jjuese.201605108

• 地质与资源 • 上一篇    下一篇

内蒙古额尔古纳地区八大关铜钼矿床流体包裹体特征与成矿时代

王晰1,2, 段明新3, 任云生1, 侯召硕4, 孙德有1, 郝宇杰1   

  1. 1. 吉林大学地球科学学院, 长春 130061;
    2. 吉林大学应用技术学院, 长春 130022;
    3. 武警黄金第三支队, 哈尔滨 150069;
    4. 吉林省地质调查院, 长春 130061
  • 收稿日期:2015-10-20 出版日期:2016-09-26 发布日期:2016-09-26
  • 通讯作者: 任云生(1969-),男,教授,博士生导师,主要从事矿床学以及矿产普查与勘探的教学与研究工作,E-mail:renys@jlu.edu.cn E-mail:renys@jlu.edu.cn
  • 作者简介:王晰(1979-),男,讲师,博士研究生,主要从事矿床学的教学与研究工作,E-mail:xiwang@jlu.edu.cn
  • 基金资助:

    中国地质调查局项目（1212011121081）；中国核工业地质局项目（201151）

Characteristics of Fluid Inclusions and Mineralization Age of Badaguan Cu-Mo Deposit in Erguna Area, Inner Mongolia

Wang Xi1,2, Duan Mingxin3, Ren Yunsheng1, Hou Zhaoshuo4, Sun Deyou1, Hao Yujie1   

  1. 1. College of Earth Sciences, Jilin University, Changchun 130061, China;
    2. Applied Technology College, Jilin University, Changchun 130022, China;
    3. No.3 Gold Geological Party of CAPF, Harbin 150069, China;
    4. Jilin Institute of Geology Survey, Changchun 130061, China
  • Received:2015-10-20 Online:2016-09-26 Published:2016-09-26
  • Supported by:

    Supported by the China Geological Survey Project (1212011121081);China's Nuclear Industry Geological Survey Project (201151)

PDF (PC)

370

摘要：

八大关铜钼矿床为内蒙古额尔古纳地区发现较早但研究程度较低的典型斑岩型矿床。为确定其成矿机制、形成时代和构造背景，对主成矿阶段矿石脉石英中的流体包裹体开展了岩相学、显微测温、气相组分的激光拉曼光谱分析，利用LA-ICP-MS锆石U-Pb法和辉钼矿Re-Os法分别测定了成矿石英闪长斑岩体和铜钼矿石的同位素年龄。结果表明：八大关铜钼矿床成矿流体为中高温、中低盐度、中低密度的NaCl-H2O-CO2±CH4流体体系，流体的沸腾作用是矿床形成的重要机制；成矿石英闪长斑岩体的锆石U-Pb同位素年龄的加权平均值为（217.6±2.6）Ma，矿石中辉钼矿的Re-Os模式年龄为（222.4±3.3）Ma，因此八大关矿床的成岩成矿作用发生于晚三叠世。综合本文获得的成岩成矿年龄及前人在区域构造演化方面的研究资料认为，八大关矿床形成于与洋壳俯冲有关的活动大陆边缘构造背景，与蒙古-鄂霍茨克洋向南俯冲所引起的构造-岩浆活动具有密切的成因联系。

关键词: 流体包裹体, 同位素测年, 矿床成因, 构造背景, 八大关铜钼矿床, 内蒙古额尔古纳地区

Abstract:

The Badaguan porphyry copper-molybdenum deposit was discovered early, but has been low-degree researched. To determine its ore-forming fluid and mineralization mechanism, fluid inclusions in quartz grains from the ore are analyzed, including petrographic characteristics, microthermometry and gas compontents. LA-ICP-MS zircon U-Pb dating of metallogenic quartz diorite porphyry and Re-Os isotopic dating of molybdenite mineral have been carried out. The Badaguan deposit is charactered by the veinlet, network and veinlet-disseminated mineralization and facial zonation of wall-rock alterations, which are similar with those of the porphyry deposits. The ore-forming fluid is of medium- low-density, medium-low-salinity, medium-high-temperature NaCl-H2O-CO2±CH4 fluid system, fluid boiling might be an important mechanism for the formation of mineral deposits. Weighted mean U-Pb age of zircon grains from the metallogenic quartz diorite porphyry is (217.6±2.6)Ma, and Re-Os model age of the molybdenite is (222.4±3.3)Ma, which indicates that the metallogenic intrusion and associated copper-molybdenum mineralization took place in Late Triassic. Moreover, according to the geochemical characteristics and previous data in tectonic environment of the metallogenic porphyry in this area, authors propose that the Badaguan deposit may be resulted from tectonic-magmatism induced by southward subduction of the Mongolia-Okhotsk ocean. These conclusions are very significant for discussion of regional metallogenic regularities and metallogeny in board area among China, Russia and Mongolia.

Key words: fluid inclusion, isotopic dating, ore genesis, tectonic setting, Badaguan Cu-Mo deposit, Erguna area in Inner Mongolia

中图分类号: 

  • P618.41

[1] 赵明玉, 王大平, 田世良. 得尔布干成矿带中段八大关-新峰山成矿地质条件分析[J].矿产与地质, 2002, 16(89):70-73. Zhao Mingyu, Wang Daping, Tian Shiliang. Metallogeny of Badaguan-Xinfengshan in the Middle Section of Derbugan Metalloginic Zone[J]. Mineral Resources and Geology, 2002, 16(89):70-73.

[2] 武广. 大兴安岭北部区域成矿背景与有色、贵金属矿床成矿作用[D]. 长春:吉林大学, 2005. Wu Guang. Metallogenic Setting and Metallogenesis of Nonferrous-Precious Metals in Northen Da Hinggan Moutain[D]. Changchun:Jilin University, 2005.

[3] 李诺, 孙亚莉, 李晶, 等. 内蒙古乌奴格吐山斑岩铜钼矿辉钼矿铼锇等时线年龄及其成矿地球动力学背景[J]. 岩石学报, 2007, 23(11):2881-2888. Li Nuo, Sun Yali, Li Jing, et al. Molybdenite Re/Os Isochron Age of the Wunugetu Shan Porphyry Cu/Mo Deposit, Inner Mongolia and Its Implication for Metallogenic Geodynamics[J]. Acta Petrologica Sinca, 2007, 23(11):2881-2888.

[4] 陈志广, 张连昌, 卢百志, 等. 内蒙古太平川铜钼矿成矿斑岩时代、地球化学特征及地质意义[J]. 岩石学报, 2010, 26(5):1437-1449. Chen Zhiguang, Zhang Lianchang, Lu Baizhi, et al. Geochronology and Geochemistry of the Taipingchuan Copper-Molybdenite Deposit in Inner Mongolia, and Its Geological Significances[J]. Acta Petrologica Sinca, 2010, 26(5):1437-1449.

[5] Wu F Y, Sun D Y, Ge W C, et al. Geochronology of the Phanerozoic Granitoids in Northeastern China[J]. Journal of Asian Earth Sciences, 2011, 41(1):1-30.

[6] 武广, 孙丰月, 赵财胜, 等. 额尔古纳地块北缘早古生代后碰撞花岗岩的发现及其地质意义[J]. 科学通报, 2005, 50(20):2278-2288. Wu Guang, Sun Fengyue, Zhao Caisheng, et al. Granite After Collision Discovery and Geological Significance of Early Paleozoic in Northern Margin of Erguna Block[J]. Chinese Science Bulletin, 2005, 50(20):2278-2288.

[7] 徐美君, 许文良, 孟恩, 等. 内蒙古东北部额尔古纳地区上护林-向阳盆地中生代火山岩LA-ICP-MS锆石U-Pb年龄和地球化学特征[J]. 地质通报, 2011, 30(9):1321-1338. Xu Meijun, Xu Wenliang, Meng En, et al. LA-ICP-MS Zircon U-Pb Chronology and Geochemistry of Mesozoic Volcanic Rocks from the Shanghulin-Xiangyang Basin in Erguna Area, Northern Inner Mongolia[J]. Geological Bulletin of the China, 2011, 30(9):1321-1338.

[8] 吴福元, 孙德有, 林强. 东北地区显生宙花岗岩的成因与地壳增生[J]. 岩石学报, 1999, 15(2):181-189. Wu Fuyuan, Sun Deyou, Lin Qiang. Petrogenesis of the Phanerozoic Granites and Crustal Growth in Northeast China[J]. Acta Petrologica Sinca, 1999, 15(2):181-189.

[9] 吕志成, 段国正, 郝立波, 等. 满洲里-额尔古纳地区岩浆作用及其大地构造意义[J]. 矿物岩石, 2001, 21(1):77-85. Lü Zhicheng, Duan Guozheng, Hao Libo, et al. Magmatism and Its Tectonic Significance in the Manzhouli-Erguna Region[J]. Mineral Petrol, 2001, 21(1):77-85.

[10] 柳晓明, 高山, 袁红林, 等. 193nm LA-ICPMS对国际地质标准参考物质中42种主量和微量元素的分析[J]. 岩石学报, 2002, 18(3):408-418. Liu Xiaoming, Gao Shan, Yuan Honglin, et al. Analysis of 42 Major and Trace Elements in Glass Standard Reference Materials by 193nm LA-ICPMS[J]. Acta Petrologica Sinca, 2002, 18(3):408-418.

[11] 袁洪林, 吴福元, 高山, 等. 东北地区新生代侵入体的锆石激光探针U-Pb年龄测定与稀土元素成分分析[J]. 科学通报, 2003, 48(14):1511-1520. Yuan Honglin, Wu Fuyuan, Gao Shan, et al. Analysis of Zircon U-Pb Age of Laser Probe in Northeast Area of Cenozoic Intrusions and Determination of Rare Earth Elements[J]. Chinese Science Bulletin, 2003, 48(14):1511-1520.

[12] 杜安道, 赵敦敏, 王淑贤. Carius管溶样-负离子热表面电离质谱准确测定辉钼矿铼-锇同位素地质年龄[J]. 岩矿测试, 2001, 20(4):247-252. Du Andao, Zhao Dunmin, Wang Shuxian. Precise Re-Os Dating for Molybdenite by ID-NTIMS with Carius Tube Sample Preparation[J]. Rock and Mineral Analysis, 2001, 20(4):247-252.

[13] 屈文俊, 杜安道. 高温密闭溶样电感耦合等离子体质谱准确测定辉钼矿铼-锇地质年龄[J]. 岩矿测试, 2003, 22(4):254-262. Qu Wenjun, Du Andao. The Electrochemical Behavior of Dopamine on Poly(Cinchomeronic Acid) Modified Glassy Carbon Electrode and Its Detection[J]. Rock and Mineral Analysis, 2003, 22(4):254-262.

[14] 王明艳, 何玲. 内蒙古查木罕钨钼多金属矿床辉钼矿Re-Os同位素年龄及其地质意义[J].大地构造与成矿学, 2013, 37(1):49-56. Wang Mingyan, He Ling. Re-Os Dating of Molybdenites from Chamuhan W-Mo Deposit, Inner Mongolia and Its Geological Implications[J]. Geotectonica et Metallogenia, 2013, 37(1):49-56.

[15] 蒋少涌, 杨竞红, 赵葵东, 等. 金属矿床Re-Os同位素示踪与定年研究[J]. 南京大学学报(自然科学), 2000, 36(6):669-677. Jiang Shaoyong, Yang Jinghong, Zhao Kuidong, et al. Re-Os Isotope Tracer and Dating Methods in Ore Deposits Research[J]. Journal of Nanjing University (Natural Sciences), 2000, 36(6):669-677.

[16] Hall D L, Sterner S M, Bodnar R J. Freezing Point Depression of NaCl-KCl-H2O Solutions[J]. Econ Geol, 1988, 83:197-202.

[17] Roedder E. Fluid inclusions[J]. Reviews in Minera-logy(Mineral Soc Amer), 1984, 12:644.

[18] 吴元保, 郑永飞. 锆石成因矿物学研究及其对U-Pb年龄解释的制约[J]. 科学通报, 2004, 49(16):1589-1604. Wu Yuanbao, Zheng Yongfei. Genesis of Zircon and Its Constraints on Interpretation of U-Pb Age[J]. Chinese Science Bulletin, 2004, 49(16):1589-1604.

[19] 李长民. 锆石成因矿物学及锆石微区定年综述[J]. 地质调查与研究, 2009, 33(3):161-174. Li Changmin. A Review on the Minerageny and Situ Microanalytical Dating Techniques of Zircons[J]. Geological Survey and Research, 2009, 33(3):161-174.

[20] 刘斌, 段光贤. NaCl-H2O溶液包裹体的密度式和等容式及其应用[J]. 矿物学报, 1987, 7(4):345-352. Liu Bin, Duan Guangxian. The Density and Isochoric Formulate for NaCl-H2O Fluid Inclusions (Salinity ≤ 25%) and Their Applications[J]. Acta Mineralogica Sinica, 1987, 7(4):345-352.

[21] 邵洁连. 金矿找矿矿物学[M]. 武汉:中国地质大学出版社, 1990:1-150. Shao Jielian. Prospecting Mineralogy of Gold Deposit[M]. Wuhan:China University of Geosciences Press, 1990:1-150.

[22] 卢焕章, 范宏瑞, 倪培, 等. 流体包裹体[M]. 北京:科学出版社, 2004:205-214. Lu Huanzhang, Fan Hongrui, Ni Pei, et al. Fluid Inclusion[M]. Beijing:Science Press, 2004:205-214.

[23] 芮宗瑶, 李荫清, 王龙生, 等. 从流体包裹体研究探讨金属矿床成矿条件[J]. 矿床地质, 2003, 22(1):13-23. Rui Zongyao, Li Yinqing, Wang Longsheng, et al. Approach to Ore-Forming Conditions in Light of Ore Fluid Inclusions[J]. Mineral Deposits, 2003, 22(1):13-23.

[24] 万多, 王可勇, 李文昌, 等. 滇西北热林Cu-Mo矿床流体包裹体特征[J]. 吉林大学学报(地球科学版), 2012, 42(增刊.3):54-63. Wan Duo, Wang Keyong, Li Wenchang, et al. Characteristics of Fluid Inclusion of Relin Cu-Mo Deposit in Northwest Yunnan Province[J]. Journal of Jilin University (Earth Science Edition), 2012, 42(Sup.3):54-63.

[25] 许庆林, 孙丰月, 张晗, 等. 山西中条山铜矿峪铜矿流体包裹体、锆石U-Pb年龄、Hf同位素及其地质意义[J]. 吉林大学学报(地球科学版), 2012, 42(增刊.3):64-80. Xu Qinglin, Sun Fengyue, Zhang Han, et al. Fluid Inclusions, Zircon U-Pb Age and Hf Isotope of Tongkuangyu Copper Deposit in Zhongtiaoshan Mountains and Its Geological Significance, Shanxi Province, China[J]. Journal of Jilin University (Earth Science Edition), 2012, 42(Sup.3):64-80.

[26] 张勇, 孙景贵, 邢树文, 等. 吉林省新华龙钼矿床流体包裹体[J]. 吉林大学学报(地球科学版), 2013, 43(6):1878-1888. Zhang Yong, Sun Jinggui, Xing Shuwen, et al. Fluid Inclusions in the Xinhualong Molybdenum Deposit, Jilin Province[J]. Journal of Jilin University (Earth Science Edition), 2013, 43(6):1878-1888.

[27] Drummond S E,Ohmoto H.Chemical Evolution and Mineral Deposition in Boiling Hydrothermal Systems[J]. Economic Geology, 1985, 80(1):126-147.

[28] 张德会. 流体的沸腾和混合在热液成矿中的意义[J]. 地球科学进展, 1997, 12(6):546-552. Zhang Dehui. Some New Advances in Ore-Forming Fluid Geochemistry on Boiling and Mixing of Fluids During the Processes of Hydrothermal Deposit[J]. Advance in Earth Sciences, 1997, 12(6):546-552.

[29] 秦克章, 李惠民, 李伟实. 内蒙古乌奴格吐山斑岩铜钼矿床的成岩、成矿时代[J]. 地质论评, 1999, 45(2):180-185. Qin Kezhang, Li Huimin, Li Weishi. Intrusion and Mineralization Ages of the Wunugetushan Porphyry Cu-Mo Deposit, Inner Mongolia, Northwest China[J]. Geological Review, 1999, 45(2):180-185.

[30] 江思宏, 聂凤军, 苏永江, 等. 蒙古国额尔登特特大型铜-钼矿床年代学与成因研究[J]. 地球学报, 2010, 31(3):289-306. Jiang Sihong, Nie Fengjun, Su Yongjiang, et al. Geochonology and Origin of the Erdenet Superlarge Cu-Mo Deposit in Mongolia[J]. Acta Geoscientica Sinica, 2010, 31(3):289-306.

[31] 孙德有, 吴福元, 张艳斌, 等. 西拉木伦河-长春-延吉板块缝合带的最后闭合时间:来自吉林大玉山花岗岩体的证据[J]. 吉林大学学报(地球科学版), 2004, 34(2):174-181. Sun Deyou, Wu Fuyuan, Zhang Yanbin, et al. The Final Closing Time of the West Lamulun River-Changchun-Yanji Plate Suture Zone:Evidence from the Day ushan Granitic Pluton, Jilin Province[J]. Journal of Jilin University (Earth Science Edition), 2004, 34(2):174-181.

[32] 李锦轶, 高立明, 孙桂华, 等. 内蒙古东部双井子中三叠世同碰撞壳源花岗岩的确定及其对西伯利亚与中朝古板块碰撞时限的约束[J]. 岩石学报, 2007, 23(3):565-582. Li Jinyi, Gao Liming, Sun Guihua, et al. Shuangjingzi Middle Triassic Syn-Collisional Crust-Derived Granite in the East Inner Mongolia and Its Constraint on the Timing of Collision Between Siberian and Sino-Korean Paleo-Plates[J]. Acta Petrologica Sinca, 2007, 23(3):565-582.

[33] 刘永江, 张兴洲, 迟效国, 等. 大兴安岭地区上古生界变形特征及构造层划分[J]. 吉林大学学报(地球科学版), 2011, 41(5):1304-1313. Liu Yongjiang, Zhang Xingzhou, Chi Xiaoguo, et al. Deformation and Tectonic Layer Division of the Upper Paleozoic in Daxing'anling Area[J]. Journal of Jilin University (Earth Science Edition), 2011, 41(5):1304-1313.

[34] 彭玉鲸, 陈跃军. 吉黑造山带与华北地台开原-山城镇段构造边界位置[J]. 世界地质, 2007, 26(1):1-6. Peng Yujing, Chen Yuejun. Location of Structureal Boundary Between Ji-Hei Orogenic Zone and Kaiyuan-Shanchen Town Section of North China Platform[J]. Global Geology, 2007, 26(1):1-6.

[35] Xu W L, Ji W Q, Pei F P, et al. Triassic Volcanism in Eastern Heilongjiang and Jilin Provinces, NE China:Chronology, Geochemistry and Tectonic Implications[J]. Journal of Asian Earth Sciences, 2009, 34(3):392-402.

[36] 许文良, 王枫, 裴福萍, 等. 中国东北中生代构造体制与区域成矿背景:来自中生代火山岩组合时空变化的制约[J]. 岩石学报, 2013, 29(2):339-353. Xu Wenliang, Wang Feng, Pei Fuping, et al. Mesozoic Tectonic Regimes and Regional Ore-Forming Background in NE China:Constraints from Spatial and Temporal Variations of Mesozoic Volcanic Rock Associations[J]. Acta Petrologica Sinca, 2013, 29(2):339-353.

[37] 裴福萍, 许文良, 杨德彬, 等. 华北克拉通东北缘岩石圈深部物质组成的不均一性:来自吉林南部中生代火山岩元素及Sr-Nd同位素地球化学的证据[J]. 岩石学报, 2009, 25(8):1962-1974. Pei Fuping, Xu Wenliang, Yang Debin, et al. Heterogeneity of Late Mesozoic Deep Lithosphere Beneath the Northeastern North China Craton:Evidence from Elemental and Sr-Nd Isotopic Geochemistry of Mesozoic Volcanic Rock in the Southern Jilin Province, China[J]. Acta Petrologica Sinca, 2009, 25(8):1962-1974.

[38] 唐杰, 许文良, 王枫, 等. 张广才岭帽儿山组双峰式火山岩成因:年代学与地球化学证据[J]. 世界地质, 2011, 30(4):508-520. Tang Jie, Xu Wenliang, Wang Feng, et al. Petrogenesis of Bimodal Volcanic Rocks from Maoershan Formation in Zhangguangcai Range:Evidence from Geochronology and Geochemistry[J]. Global Geology, 2011, 30(4):508-520.

[39] Yu J J, Wang F, Xu W L, et al. Early Jurassic Mafic Magmatism in the Lesser Xing'an-Zhangguangcai Range, NE China, and Its Tectonic Implications:Constrains from Zircon U-Pb Chronology and Geochemistry[J]. Lithos, 2012(142/143):256-266.

[40] 徐美君, 许文良, 王枫, 等. 小兴安岭西北部早侏罗世花岗质岩石的年代学与地球化学及其构造意义[J]. 岩石学报, 2013, 29(2):354-368. Xu Meijun, Xu Wenliang, Wang Feng, et al. Geochronology and Geochemistry of the Early Jurassic Granitoids in the Central Lesser Xing'an Range, NE China and Its Tectonic Implications[J]. Acta Petrologica Sinca, 2013, 29(2):354-368.

[41] Zonenshain L P, Kuzmin M L, Natapov L M. Geology of the USSR:A Plate-Tectonics Synthesis[C]. Washington D C:American Geophysical Union, Geodynamics Series, 1990:1-242.

[42] Zorin Y A.Geodynamics of the Western Part of the Mongolia-Okhotsk Collisional Belt, Trans-Baikal Region (Russia) and Mongolia[J]. Tectonophysics, 1999, 306(1):33-56.

[43] 莫申国, 韩美莲, 李锦铁. 蒙古-鄂霍茨克造山带的组成及造山过程[J]. 山东科技大学学报(自然科学版), 2005, 24(3):50-52. Mo Shenguo, Han Meilian, Li Jinyi. Compositions and Orogenic Processes of Mongolia-Okhotsk Orogen[J]. Journal of Shandong University of Science and Technology (Natural Science), 2005, 24(3):50-52.

[44] Mazukabzov A M, Donskaya T V, Gladkochub D P, et al. The Late Paleozoic Geodynamics of the West Transbaikalian Segment of the Central Asian Fold Belt[J]. Russian Geology and Geophysics, 2010, 51(5):482-491.

[45] 吕志成, 段国正, 郝立波, 等. 北方造山带东北段中生代构造-流体-成岩成矿体系及其演化[J]. 大地构造与成矿学, 2010, 25(2):161-170. Lü Zhicheng, Duan Guozheng, Hao Libo, et al. The Interaction System Between Mesozoic Tectonic, Fluid,Petrogenesis and Mineralization in the Northeast of the Northern Orogenic Belt, China[J]. Geotectonica et Metallogenia, 2010, 25(2):161-170.

[46] 徐贵忠, 边千韬, 王艺芬. 额尔古纳造山带构造演化与成矿作用[J]. 地质科学, 1998, 33(1):84-92. Xu Guizhong, Bian Qiantao, Wang Yifen. Tectonic Evolution and Metallization of the Erguna Orogenic Belt[J]. Chinese Journal of Geology, 1998, 33(1):84-92.

[47] 孙燕, 刘建明, 曾庆栋. 斑岩型铜(钼)矿床和斑岩型钼(铜)矿床的形成机制探讨:流体演化及构造背景的影响[J]. 地学前缘, 2012, 19(6):179-193. Sun Yan, Liu Jianming, Zeng Qingdong. An Approach to Metallogenic Mechanism of Porphyry Copper (Molybdenum) Deposits and Porphyry Molybdenum (Copper) Deposits:Influence of Evolving Processes of Ore-Forming Fluids and Tectonic Settings[J]. Earth Science Frontiers, 2012, 19(6):179-193.

[48] Mikhail I, Kuzmin, Victor S A. Geochemical Types of Granitoids of the Mongol-Okhotsk Belt and Their Geodynamic Settings[J]. Chinese Journal of Geochemistry, 1999, 12(2):110-117.

[49] 张连昌, 陈志广, 吴华英, 等. 蒙古-鄂霍茨克造山带得尔布干多金属成矿带构造-岩浆成矿作用及动力学背景[J]. 矿床地质, 2010, 29(增刊):125-126. Zhang Lianchang, Chen Zhiguang, Wu Huaying, et al. Tectonic-Magmatic Mineralization and Dynamics Background of Derbugan Polymetallic Metallogenic Belt in Mongolia-Okhotsk Orogen[J]. Mineral Deposits, 20100, 29(Sup.):125-126.

[50] 唐文龙, 李俊建, 王国明. 中蒙边境及邻区典型斑岩型铜矿地球化学特征概述[J]. 地质调查与研究, 2009, 33(2):98-104. Tang Wenlong, Li Junjian, Wang Guoming. Geochemical Features of the Typical Porphyry Copper Deposit in China-Mongolia Border and Its Neighbor Area[J]. Geological Survey and Research, 2009, 33(2):98-104.
[1] 李向文, 张志国, 王可勇, 孙加鹏, 杨吉波, 杨贺. 大兴安岭北段宝兴沟金矿床成矿流体特征及矿床成因[J]. 吉林大学学报(地球科学版), 2018, 48(4): 1071-1084.
[2] 李文强, 郭巍, 孙守亮, 杨绪海, 刘帅, 侯筱煜. 塔里木盆地巴楚—麦盖提地区古生界油气藏成藏期次[J]. 吉林大学学报(地球科学版), 2018, 48(3): 640-651.
[3] 陈瑞莉, 陈正乐, 伍俊杰, 梁志录, 韩凤彬, 王永, 肖昌浩, 韦良喜, 沈滔. 甘肃合作早子沟金矿床流体包裹体及硫铅同位素特征[J]. 吉林大学学报(地球科学版), 2018, 48(1): 87-104.
[4] 和成忠, 张德会, 吴鸣谦, 夏岩, 张荣臻, 胡铁军. 辽宁青城子姚家沟斑岩型钼矿流体包裹体[J]. 吉林大学学报(地球科学版), 2017, 47(6): 1717-1731.
[5] 门兰静, 孙景贵, 王好均, 柴鹏, 赵克强, 古阿雷, 刘城先. 延边浅成高硫化热液金矿床的成矿流体起源与演化:以杜荒岭和九三沟矿床为例[J]. 吉林大学学报(地球科学版), 2017, 47(5): 1365-1382.
[6] 陈晶源, 王长明, 贺昕宇, 陈良, 吴彬, 王乔, 张端, 姚恩亚, 董猛猛. 河南瓦房铅锌矿床地质、流体包裹体和稳定同位素特征[J]. 吉林大学学报(地球科学版), 2017, 47(5): 1383-1404.
[7] 张艳, 韩润生, 魏平堂, 邱文龙. 云南会泽矿山厂铅锌矿床流体包裹体特征及成矿物理化学条件[J]. 吉林大学学报(地球科学版), 2017, 47(3): 719-733.
[8] 郝立波, 赵昕, 赵玉岩. 辽宁白云金矿床稳定同位素地球化学特征及矿床成因[J]. 吉林大学学报(地球科学版), 2017, 47(2): 442-451.
[9] 赵彦德, 齐亚林, 罗安湘, 程党性, 李继宏, 黄锦绣. 应用流体包裹体和自生伊利石测年重构鄂尔多斯盆地侏罗系油藏烃类充注史[J]. 吉林大学学报(地球科学版), 2016, 46(6): 1637-1648.
[10] 王力, 孙丽伟. 山东省寺庄金矿床成矿流体特征[J]. 吉林大学学报(地球科学版), 2016, 46(6): 1697-1710.
[11] 李福来, 肖飞, 孟凡超, 任泽樱. 内蒙古索伦地区上二叠统林西组碎屑岩地球化学特征及其对物源的指示意义[J]. 吉林大学学报(地球科学版), 2016, 46(6): 1769-1780.
[12] 张延军, 孙丰月, 李碧乐, 李良, 陈扬. 青海湟中县三岔金矿流体包裹体特征及矿床成因[J]. 吉林大学学报(地球科学版), 2016, 46(5): 1342-1353.
[13] 温志良, 姜福平, 钟长林, 姜雪飞, 王果谦, 齐岩. 松辽盆地东南隆起超大型油页岩矿床特征及成因[J]. 吉林大学学报(地球科学版), 2016, 46(3): 681-691.
[14] 吴海枝, 韩润生, 吴鹏. 楚雄盆地六苴砂岩型铜矿床成矿流体性质及演化[J]. 吉林大学学报(地球科学版), 2016, 46(2): 398-411.
[15] 曾令高, 张均, 孙腾, 李斌, 朱光辉, 贾子超, 方权, 陈庚户. 峨眉山大火成岩省烂纸厂铁矿床地质特征、成因及其找矿勘查启示[J]. 吉林大学学报(地球科学版), 2016, 46(2): 412-424.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
No Suggested Reading articles found!
版权所有 © 《吉林大学学报(地球科学版)》编辑部
地址：长春市西民主大街938号(130026)　电话：+86-431-88502374；13756165364　E-mail: xuebao1956@jlu.edu.cn
本系统由北京玛格泰克科技发展有限公司设计开发