吉林大学学报(地球科学版) ›› 2015, Vol. 45 ›› Issue (1): 119-131.doi: 10.13278/j.cnki.jjuese.201501110

• 地质与资源 • 上一篇    下一篇

福建连城铜坑钼矿床辉钼矿Re-Os同位素年龄及燕山期成矿事件

王少怀, 黄宏祥   

  1. 福州大学紫金矿业学院, 福州 350108
  • 收稿日期:2014-03-20 发布日期:2015-01-26
  • 作者简介:王少怀(1965), 男, 教授, 博士, 主要从事矿产普查与勘探的教学和科研工作, E-mail:wangsh@fzu.edu.cn
  • 基金资助:

    福建省自然科学基金项目(2012J01172);国土资源部典型金属矿科学基地研究(建设)项目(200911007);国家自然科学基金项目(41172041)

Re-Os Isotopic Dating of Molybdenite and the Yanshanian Mineralization of the Tongkeng Molybdenum Deposit in Liancheng, Fujian Province

Wang Shaohuai, Huang Hongxiang   

  1. Zijin College of Mining, Fuzhou University, Fuzhou 350108, China
  • Received:2014-03-20 Published:2015-01-26

摘要:

福建连城铜坑钼矿床是近年来在闽西南地区找到的又一处钼矿床。钼矿化在铜坑燕山晚期第一阶段花岗斑岩岩体与晚古生界变质岩接触带内呈浸染状、脉状、透镜状等形态产出。本次研究过程中, 对6件代表性辉钼矿样品进行了Re-Os同位素年龄测定, Re-Os同位素模式年龄值为115.1~116.7 Ma, 等时线年龄为(115.7±1.1) Ma, 由此认为铜坑钼矿床与花岗斑岩的形成时间均为早白垩世, 属燕山晚期构造-岩浆活动的产物。结合矿区外围其他钼矿床同位素年龄数据可以推测, 闽西南坳陷燕山早期大规模钼矿化发生在印支期稳定的台地向活动大陆边缘转变阶段并伴随燕山早期挤压隆升(160~145 Ma), 燕山晚期由挤压向拉张机制转换(125~105 Ma)的构造改造阶段所诱发的岩浆活动是导致钼矿床形成的主导因素。

关键词: 地质学, Re-Os同位素, 辉钼矿, 成矿年龄, 连城铜坑钼矿床, 福建

Abstract:

Located in the southwestern Fujian Province, the Tongkeng ore deposit in Liancheng is a newly discovered molybdenum deposit. The molybdenum mineralization occurs within the contact zone between the granite porphyry stock formed in the first stage of late Yanshanian magmatic event in Tongkeng area and late Paleozoic metamorphic rocks. Ore bodies are charactered by vein, veinlet and disseminated. Re-Os dating of six molybdenite samples collected from the major ore body shows that the isochron age is (115.7±1.1) Ma and the model ages range from 115.1 Ma to 116.7 Ma, with an average value of (115.8±0.8) Ma. It can be considered that both the granite-porphyry and associated molybdenum mineralization were formed in Early Cretaceous, and that both were derived by the late Yanshanian tectonic-magmatic event in the southwestern Fujian depression. Combined with isotopic age data from other adjacent molybdenum deposits, it can be inferred that the early Yanshanian large-scale molybdenum mineralization in the southwestern Fujian depression formed during the transition stage from the Indosinian sustained platform to active continental margin, and accompanied by compressing and uplifting in early Yanshanian (about 160-145 Ma);the late Yanshanian tectonic conversion from compressing to tension (about 125-105 Ma) resulted in the magmatism which seemed to be the dominant factor for the late Yanshanian molybdenum deposit.

Key words: geology, Re-Os isotope, molybdenite, metallogenic age, Tongkeng molybdenum deposit in Liancheng, Fujian

中图分类号: 

  • P618.65

[1] 侯增谦, 潘小菲, 杨志明, 等.初论大陆环境斑岩铜矿[J].现代地质, 2007, 21(2):332-351. Hou Zengqian, Pan Xiaofei, Yang Zhiming, et al.Porphyry Cu-(Mo-Au) Deposits no Related to Oceanic-Slab Subduction:Examples from Chinese Porphyry Deposits in Continental Settings[J].Geoscience, 2007, 21(2):332-351.

[2] 夏斌, 陈根文, 王核.全球超大型斑岩铜矿床形成的构造背景分析[J].中国科学:D辑, 2002, 32(增刊):87-95. Xia Bin, Chen Genwen, Wang He.Analysis of Tectonic Setting of Global Superlarge Porphry Copper Deposit[J].Science in China:Series D, 2002, 32(Sup.):87-95.

[3] Oyarzun R, Marques A, Lillo J, et al.Giant Versus Small Porphyry Copper Deposits of Cenozoic Age in Northern Chile:Adakitic Versus Normal Calc-Alkaline Magmatism[J].Mineralium Deposits, 2001, 36:794-798.

[4] 芮宗瑶, 张洪涛, 陈仁义, 等.斑岩铜矿研究中若干问题探讨[J].矿床地质, 2006, 25(4):491-500. Rui Zongyao, Zhang Hongtao, Chen Renyi, et al.An Approach to Some Problems of Porphyry Copper Deposits[J].Mineral Deposits, 2006, 25(4):491-500.

[5] 王少怀, 裴荣富, 曾宪辉, 等.再论紫金山矿田成矿系列和成矿模式[J].地质学报, 2009, 83(2):145-157. Wang Shaohuai, Pei Rongfu, Zeng Xianhui, et al.Metallogenic Series and Model of the Zijinshan Mining Field[J].Acta Geologica Sinica, 2009, 83(2):145-157.

[6] 王少怀.紫金山矿集区地球化学异常特征及找矿潜力预测[J].大地构造与成矿学, 2011, 35(1):156-160. Wang Shaohuai.Characteristics of Gold Geochemical Anomalies and Ore Potential Forecasting of the Zijinshan Area of Extensive Gold Mineralization[J].Geotectonica et Metallogenia, 2011, 35(1):156-160.

[7] 王绍雄.福建省寻找大型斑岩铜矿的前景与途径[J].福建地质, 1995, 14(4):165-176. Wang Shaoxiong.Future and Way of Searching for the Large-Sized Porphyry Copper Deposits in Fujian Province[J].Geology of Fujian, 1995, 14(4):165-176.

[8] 罗锦昌, 陈郑辉, 屈文俊.福建省永定山口钼矿辉钼矿铼-锇同位素定年及其地质特征[J].岩矿测试, 2009, 28(3):254-258. Luo Jinchang, Chen Zhenghui, Qu Wenjun.Re-Os Isotopic Dating of Molybdenite from the Shankou Molybdenum Deposit in Yongding County of Fujian Province and Its Geological Significance[J].Rock and Mineral Analysis, 2009, 28(3):254-258.

[9] 张达, 吴淦国, 刘乃忠, 等.福建漳平北坑场钼多金属矿床辉钼矿Re-Os同位素年龄及其地质意义[J].地质学报, 2010, 84(10):1428-1437. Zhang Da, Wu Ganguo, Liu Naizhong, et al.Re-Os Isotopic Age of Molybdenite from the Beikengchang Molybdenite and Polymetal Deposit in Zhangping City, Fujian Province and Its Geological Significance[J].Acta Geologica Sinica, 2010, 84(10):1428-1437.

[10] 张家菁, 陈郑辉, 王登红, 等.福建行洛坑大型钨矿的地质特征、成矿时代及其找矿意义[J].大地构造与成矿学, 2008, 32(1):92-97. Zhang Jiajing, Chen Zhenghui, Wang Denghong, et al.Geological Characteristics and Metallogenic Epoch of the Xingluokeng Tungsten Deposit, Fujian Province[J].Geotectonica et Metalbgenia, 2008, 32(1):92-97.

[11] 张承帅, 毛景文, 谢桂青, 等.福建马坑矽卡岩型铁(钼)矿床地质特征及辉钼矿Re-Os同位素年龄[J].吉林大学学报:地球科学版, 2012, 42(增刊1):224-236. Zhang Chengshuai, Mao Jingwen, Xie Guiqing, et al.Geology and Molybdenite Re-Os Ages of Makeng Skarn-Type Fe-Mo Deposit in Fujian Province[J].Journal of Jilin University:Earth Science Edition, 2012, 42(Sup.1):224-236.

[12] 梁清玲, 江思宏, 王少怀, 等.福建紫金山矿田罗卜岭斑岩型铜钼矿床辉钼矿Re-Os定年及地质意义[J].地质学报, 2012, 86(7):1113-1119. Liang Qingling, Jiang Sihong, Wang Shaohuai, et al.Re-Os Dating of Molybdenite from the Luoboling Porphyry Cu-Mo Deposit in the Zijinshan Ore Field of Fujian Province and Its Geological Significance[J].Acta Geologica Sinica, 2012, 86(7):1113-1119.

[13] 雷广文.闽东地区钼矿床控矿因素与成矿模式探讨[J].福建地质, 2010, 29(3):194-201. Lei Guangwen.On the Ore-Controlling Factors and the Metallogenic Pattern of Molybdenum Deposits in East Fujian[J].Geology of Fujian, 2010, 29(3):194-201.

[14] 张克尧, 王建平, 杜安道, 等.福建福安赤路钼矿床辉钼矿Re-Os同位素年龄及其地质意义[J].中国地质, 2009, 36(1):147-155. Zhang Keyao, Wang Jianping, Du Andao, et al.Re-Os Isotopic Dating of Molybdenite from the Chilu Molybdenum Deposit in Fuan, Fujian Province[J].Geology in China, 2009, 36(1):147-155.

[15] 黄昌旗.福建福安赤路宁德九曲岭地区钼铜多金属矿找矿前景分析[J].福建地质, 2008, 28(4):289-295. Huang Changqi.The Study of Mo-Cu Polymetalic Deposits Prospecting Perspective in Fuan Chilu-Ningde Jiuquling District, Fujian Province[J].Geology of Fujian, 2008, 28(4):289-295.

[16] 黄文明.福建仙游砺山钼矿地质特征及成因探讨[J].福建地质, 2007, 26(2):65-71. Huang Wenming.On Geologic Characteristics and Genesis of the Lishan Molybdenum Deposit in Xianyou County of Fujian Province[J].Geology of Fujian, 2007, 26(2):65-71.

[17] 石礼炎.福建古田西朝钼矿床成矿构造特征及找矿方向[J].福建地质, 2009, 28(3):167-174. Shi Liyan.The Metallotectonic Characteristics and the Ore-Finding Target of the Xichao Molybdenum Deposit in Gutian County, Fujian Province[J].Geology of Fujian, 2009, 28(3):167-174.

[18] 李汶奎.福建省古田县西朝钼矿区成矿规律及找矿标志研究[J].湖南有色金属, 2008, 24(5):1-4. Li Wenkui.The Study on Mineralization Rule and the Prospecting Symbolized of Xichao Molybdenum Ore Area in Gutian County of Fujian Province[J].Hunan Nonferrous Metals, 2008, 24(5):1-4.

[19] 谭元松.福建永泰无岩坑钼矿地质特征及成因探讨[J].福建地质, 2010, 29(2):101-106. Tan Yuansong.Geologic Characteristics and Origin Discussion of the Wuyankeng Molybdenum Deposit in Yongtai County, Fujian Province[J].Geology of Fujian, 2010, 29(2):101-106.

[20] 杨卫立.福建周宁咸格钼矿地质特征及找矿潜力分析[J].福建地质, 2009, 28(3):175-180. Yang Weili.Geologic Characteristics and Ore-Finding Potentiality of the Xiange Molybdenum Deposit in Zhouning County, Fujian Province[J].Geology of Fujian, 2009, 28(3):175-180.

[21] 杨武平.福建霞浦大湾铍钼矿床地质特征及成因初探[J].福建地质, 2008, 27(1):1-7. Yang Wuping.On Geological Characteristics and Genesis of the Dawan Beryllium and Molybdenum Deposit in Xiapu County, Fujian Province[J].Geology of Fujian, 2008, 27(1):1-7.

[22] 钟森芳.福建屏南灵峰钼矿床地质特征及找矿初探[J].亚热带资源与环境学报, 2010, 5(2):86-91. Zhong Senfang.The Lingfeng Molybdenum Deposit in Pingnan County of Fujian Province:Geological Features and Prospecting[J].Journal of Subtropical Resources and Environment, 2010, 5(2):86-91.

[23] 傅树超.福建武夷山坪地钼矿床地质特征及成因探讨[J].福建地质, 2005, 24(3):125-133. Fu Shuchao.On Geologic Characteristics and Genesis of the Pingdi Molybdenum Deposit in Wuyishan City, Fujian Province[J].Geology of Fujian, 2005, 24(3):125-133.

[24] 傅树超.福建松溪后洋矿区钼矿地质特征[J].福建地质, 2008, 27(1):8-12. Fu Shuchao.Geologic Characteristics of the Houyang Molybdenum Deposit in Songxi County, Fujian Province[J].Geology of Fujian, 2008, 27(1):8-12.

[25] 赖文金.福建邵武观音山钼矿床地质特征及成因探讨[J].福建地质, 2010, 29(3):201-206. Lai Wenjin.On the Geological Characteristics and Genesis of the Guanyinshan Molybdenum Deposit in Shaowu, Fujian Province[J].Geology of Fujian, 2010, 29(3):201-206.

[26] 刘乃忠.福建浦城上厂钼矿床地质特征及成因初探[J].福建地质, 2005, 24(3):141-146. Liu Naizhong.On the Geologic Characteristics and Genesis of the Shangchang Molybdenum Deposit in Pucheng County, Fujian Province[J].Geology of Fujian, 2005, 24(3):141-146.

[27] 刘诗光.福建松溪大林坑钼多金属矿床地质特征及成因初探[J].福建地质, 2005, 24(1):134-140. Liu Shiguang.On the Geologic Characteristics and Genesis of the Dalinkeng Molybdenum-Polymetallic Deposit in Songxi County, Fujian Province[J].Geology of Fujian, 2005, 24(1):134-140.

[28] 王培宗, 陈耀安, 曹宝庭, 等.福建省地壳-上地慢结构及深部构造背景的研究[J].福建地质, 1993, 12(2):79-158. Wang Peizong, Chen Yaoan, Cao Baoting, et al.Crust-Upper-Mantle Structure and Deepstructural Setting of Fujian Province[J].Geology of Fujian, 1993, 12(2):79-158.

[29] Du Andao, Wu Shuqi, Sun Dezhong, et al.Preparation and Certification of Re-Os Dating Reference Materials:Molybdenite HLP and JDC[J].Geostandard and Geoanalytical Research, 2004, 28(1):41-52.

[30] 杜安道, 屈文俊, 李超, 等.铼-锇同位素定年方法及分析测试技术的进展[J].岩矿测试, 2009, 28(3):288-304. Du Andao, Qu Wenjun, Li Chao, et al.The Development of Re-Os Isotopic Dating Methods and Techniques[J].Rock and Mineralanalysis, 2009, 28(3):288-304.

[31] 杜安道, 赵敦敏, 王淑贤, 等.Carius管溶样和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, et al.Precise Re-Os Dating for Molybdenite by ID-NTIMS with Carius Tube Sample Preparation[J].Rock and Mineralanalysis, 2001, 20(4):247-252.

[32] 杜安道, 何红蓼, 殷宁万, 等.辉钼矿的铼-锇同位素地质年龄测定方法研究[J].地质学报, 1994, 68(4):339-347. Du Andao, He Hongliao, Yin Ningwan, et al.A Study on the Rhenium-Osmium Geochronometry of Mo-lybdenites[J].Acta Geologica Sinica, 1994, 68(4):339-347.

[33] 屈文俊, 杜安道, 李超, 等.金川铜镍硫化物样品中锇同位素比值的高精度分析[J].岩矿测试, 2009, 28(3):219-222. Qu Wenjun, Du Andao, Li Chao, et al.High-Precise Determination of Osmium Isotopic Ratio in the Jinchuan Copper-Nickel Sulfide Ore Samples[J].Rock and Mineral Analysis, 2009, 28(3):219-222.

[34] 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.Highly Precise Re-Os Dating of Molybdenite by ICP-MS with Carius Tube Sample Digestion[J].Rock and Mineral Analysis, 2003, 22(4):254-262.

[35] Wieser M E.Atomic Weights of the Elements(IU-PAC Technical Report)[J].Pure Appl Chem, 2006, 78(11):2051-2066.

[36] Bohlkea J K, Laeter J R, Bievre P D.Isotopic Com-positions of the Elements[J].Phys Chem Ref Data, 2005, 34(1):57-67.

[37] Smoliar M I, Walker R J, Morgan J W.Re-Os Ages of Group IIA, ⅢA, IVA and VIB Iron Meteorites[J].Science, 1996, 271:1099-1102.

[38] Ludwig K R.Isoplot for MS-DOS:A Plotting and Regression Program for Radiogenic-Isotope Data, for IBM-PC Compatible Computers, Version 1.00[M].Virginia:Geological Survey, 1988.

[39] 孟祥金, 侯增谦, 董光裕, 等.江西金溪熊家山钼矿床特征及其Re-Os年龄[J].地质学报, 2007, 81(7):946-1001. Meng Xiangjin, Hou Zengqian, Dong Guangyu, et al.The Geological Characteristics and Re-Os Isotope Age of Molybdenite of the Xiongjiashan Molybdenum Deposit, Jiangxi Province[J].Acta Geologica Sinica, 2007, 81(7):946-1001.

[40] 毛景文, 张作衡, 张招崇, 等.北祁连山小柳沟钨矿床中辉钼矿Re-Os年龄测定及其意义[J], 地质论评, 1999, 45(4):412-417. Mao Jingwen, Zhang Zuoheng, Zhang Zhaochong, et al.Re-Os Age Dating of Molybdenites in the Xiaoliugou Tungsten Deposit in the Northern Qilian Mountains and Its Significance[J].Geological Review, 1999, 45(4):412-417.

[41] 任纪舜, 牛宝贵, 和政军, 等.中国东部的构造格局和动力演化·地学研究[M]. 北京, 地质出版社, 1997. Ren Jishun, Niu Baogui, He Zhengjun, et al.Tectonic Framework and Geodynamic Evolution of Eastern China·Dixue Yanjiu[M].Beijing.Geological Publishing House, 1997.

[42] 李文达, 毛建仁, 朱云鹤, 等.中国东南部中生代火成岩与矿床[M].北京:地震出版社, 1998. Li Wenda, Mao Jianren, Zhu Yunhe, et al.The Mesozoic Igneous Rocks and Mineral Deposits in Southeastern China[M].Beijing:Seismological Publishing House, 1998.

[43] 聂童春.闽西南地区印支期隆起-伸展构造的厘定及其控矿作用[J].福建地质, 2010, 29(4):315-322. Nie Tongchun.On Confirmation of the Indo-Sinian Uplift and Extensional Structures in Southwestern Fujian and Its Control of Mineralization[J].Geology of Fujian, 2010, 29(4):315-322.

[44] 李兼海.福建省构造运动、构造层划分及其主要特征[J].福建地质, 1998, 17(3):115-130. Li Jianhai.Classification and Characteristics of the Tecnotic Movements and Structural Layersin Fujian Province[J].Geology of Fujian, 1998, 17(3):115-130.

[45] 韦德光, 揭育金, 黄廷淦.福建省区域地质构造特征[J].中国区域地质, 1997, 16(2):162-170. Wei Deguang, Jie Yujin, Huang Tinggan.Regional Geological Structure of Fujian[J].Regional Geology of China, 1997, 16(2):162-170.

[46] 冯宗帜.福建中生代火山作用与构造环境[J].中国区城地质, 1993, 12(4):311-316. Feng Zongzhi.Mesozoic Volcanism and Tectonic Environments in Fujian[J].Regional Geology of China, 1993, 12(4):311-316.

[47] 卢俊胜.福建省永定山口钼矿区地质特征及成因[J].资源调查与环境, 2008, 29(4):289-296. Lu Junsheng.Geological Characteristics and Genesis of the Shankou Molybdenum Deposit in Yongding Country, Fujian Province[J].Resources Survey & Environment, 2008, 29(4):289-296.

[48] 卢克标.福建漳平北坑场钼多金属矿地质特征及成矿模式探讨[J].福建地质, 2011, 30(1):6-11. Lu Kebiao.On the Metallogenic Pattern and the Geologic Characteristics of the Beikengchang Molybdenum Polymetallic Deposit in Zhangping City, Fujian Province[J].Geology of Fujian, 2011, 30(1):6-11.

[49] 钟军, 陈衍景, 陈静, 等.福建省紫金山矿田罗卜岭斑岩型铜钼矿床流体包裹体研究[J].岩石学报, 2011, 27(5):1410-1424. Zhong Jun, Chen Yanjing, Chen Jing, et al.Fluid Inclusion Study of the Luoboling Porphyry Cu-Mo Deposit in the Zijinshan Ore Field, Fujian Province[J].Acta Petrologica Sinica, 2011, 27( 5):1410-1424.

[50] 薛凯, 阮诗昆.福建紫金山矿田罗卜岭铜(钼)矿床地质特征及成因探讨[J], 资源环境与工程, 2008, 22(5):491-496. Xue Kai, Ruan Shikun.Geological Characteristics and Genesis of the Luobuling Copper (Molybdenum) Deposit in Zijinshan Ore Field, Fujian[J].Resources Environment & Engineering, 2008, 22(5):491-496.

[51] 苏水生.福建上杭铜矿沟萝卜岭斑岩型铜矿床地质特征及远景评价[J].福建地质, 2003, 29(2):69-77. Su Shuisheng.Geologic Characteristics and Prospective Values of the Tongkuanggou-Loboling Porphyry Copper Deposit in Shanghang County, Fujian Province[J].Geology of Fujian, 2003, 29(2):69-77.

[52] 石建基.福建武平地区晚侏罗世石英脉和云英岩型2类钼矿控矿因素及找矿方向[J].福建地质, 2010, 29(1):1-7. Shi Jianji.Ore-Controlling Factors and Prospecting Targets of Two Molybdenum Ores of the Late Jurassic Quartz-Vein and Greisen Types in Wuping County, Fujian Province[J].Geology of Fujian, 2010, 29(1):1-7.

[53] 王林昌.福建武平中赤下坝地区钨钼多金属矿找矿前景浅析[J].福建地质, 2010, 29(3):189-193. Wang Linchang.On the Ore-Finding Perspective of Tungsten and Molybdenum Polymetallic Ores in the Zhongchi-Xiaba Area of Wuping County, Fujian Province[J].Geology of Fujian, 2010, 29(3):189-193.

[54] 韩胜康.福建永定新村钼铅锌多金属矿床地质特征及成因探讨[J].福建地质, 2008, 27(4):352-360. Han Shengkang.On the Geologic Characteristics and Genesis of the Xincun Molybdenum, Lead and Zinc Polymetallic Deposit in Yongding Country, Fujian Province[J].Geology of Fujian, 2008, 27(4):352-360.

[55] 黄道锐.福建南平巨口白石岩钼矿床地质特征及成因探讨[J].福建地质, 2008, 27(3):275-280. Huang Daorui.Geologic Characteristics and Genesis of the Baishiyan Molybdenum Deposit in Nanping, Fujian Province[J].Geology of Fujian, 2008, 27(3):275-280.

[56] 林朝霞.马坑铁矿西矿段铝矿回收利用探讨[J].矿业快报, 2007, 26(9):55-57. Lin Zhaoxia.The Discussion of Recycling Aluminium Ore in West Ore Block of Makeng Iron Deposit[J].Express Information of Mining Industry, 2007, 26(9):55-57.

[57] 王少怀.福建武平十二排钼矿床辉钼矿Re-Os同位素年龄及其地质意义[J].地质论评, 2013, 59(9):885-892. Wang Shaohuai.Re-Os Isotopic Dating of Molybdenite from Shierpai Molybdenum Deposit in Wuping, Fujian and Its Geological Significance[J].Geological Review, 2013, 59(9):885-892.

[1] 耿艳光, 简伟, 李洪英, 叶会寿, 毕珉烽, 胡乔青, 李超, 范成龙, 王梦琦. 中条山篦子沟铜矿辉钼矿铼-锇同位素年龄及其地质意义[J]. 吉林大学学报(地球科学版), 2017, 47(5): 1405-1418.
[2] 段志明, 李光明, 王保弟, 李应栩, 黄勇, 郭琳, 段瑶瑶. 西藏中冈底斯成矿带查个勒铅锌矿床含矿斑岩年代学及其地质意义[J]. 吉林大学学报(地球科学版), 2015, 45(6): 1667-1690.
[3] 冯晓曦, 姚书振, 段明, 曲凯, 王佳营, 冯旭彪, 李超, 周利敏. 内蒙古白乃庙铜(钼)矿床辉钼矿Re-Os同位素年龄及其地质意义[J]. 吉林大学学报(地球科学版), 2015, 45(1): 132-141.
[4] 张勇, 孙景贵, 邢树文, 赵克强,王岩, 邱殿明,刘思宇,陈明. 吉林四方甸子钼矿床成岩成矿时代及岩石地球化学特征[J]. 吉林大学学报(地球科学版), 2014, 44(6): 1869-1882.
[5] 郝立波,吴超,孙立吉,蒋艳明,赵玉岩,陆继龙,李杰. 吉林红旗岭铜镍硫化物矿床Re-Os同位素特征及其意义[J]. 吉林大学学报(地球科学版), 2014, 44(2): 507-517.
[6] 郝宇杰,任云生,赵华雷,邹欣桐,陈聪,侯召硕,屈文俊. 黑龙江省翠宏山钨钼多金属矿床辉钼矿Re-Os同位素定年及其地质意义[J]. 吉林大学学报(地球科学版), 2013, 43(6): 1840-1850.
[7] 张志辉,张达,吴淦国,罗平,陈锡华,狄永军,吕良冀. 赣北梅子坑钼矿床辉钼矿Re-Os同位素年龄及其地质意义[J]. 吉林大学学报(地球科学版), 2013, 43(6): 1851-1863.
[8] 赵正,陈毓川,曾载淋,陈郑辉,王登红,赵斌,张家菁. 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.
[9] 邓宾, 李智武,刘树根,孙东,钟勇,李金玺,汤聪. 大巴山城口弧形断裂带右旋走滑构造特征及其意义[J]. 吉林大学学报(地球科学版), 2013, 43(5): 1501-1516.
[10] 张金树, 多吉,夏代祥,钟康惠,吴华,李光明. 西藏冈底斯驱龙斑岩型铜钼-矽卡岩型铜矿成矿体系:辉钼矿Re-Os同位素年代学证据[J]. 吉林大学学报(地球科学版), 2013, 43(5): 1366-1376.
[11] 楚亚婷,刘显凡,赵甫峰,卢秋霞,李春辉,肖继雄,吴冉,宋祥峰,蔡永文,蔡飞跃. 滇西马厂箐钼铜金矿床中赋矿斑状花岗岩定年及其地质意义[J]. 吉林大学学报(地球科学版), 2013, 43(5): 1377-1392.
[12] 黄超,余朝华,张桂林,傅良同,袁志云,范兴燕. 郯庐断裂中段新生代右行走滑位移[J]. 吉林大学学报(地球科学版), 2013, 43(3): 820-832.
[13] 戴静,孙柏年,谈树成,高博,赵志芳,王永栋. 福建永安坂头组植物及古气候分析[J]. 吉林大学学报(地球科学版), 2013, 43(1): 155-168.
[14] 谭红艳,舒广龙,吕骏超,韩仁萍,张森,寇林林. 小兴安岭鹿鸣大型钼矿LA-ICP-MS锆石U-Pb和辉钼矿Re-Os年龄及其地质意义[J]. 吉林大学学报(地球科学版), 2012, 42(6): 1757-1770.
[15] 王登红,李超,陈郑辉,王成辉,黄凡,屈文俊. 辉钼矿在矿床学研究中的新用途(I):稀土元素示踪[J]. 吉林大学学报(地球科学版), 2012, 42(6): 1647-1655.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!