吉林大学学报(地球科学版) ›› 2015, Vol. 45 ›› Issue (3): 743-758.doi: 10.13278/j.cnki.jjuese.201503109

• 地质与资源 • 上一篇    下一篇

青海祁漫塔格地区虎头崖矿床Ⅵ矿带花岗岩的成岩时代、地球化学特征和成因

姚磊1,2, 吕志成2,3, 于晓飞2,3, 庞振山2,3, 蔡煜琦4, 刘鹏5, 刘长城6, 王凤兰7   

  1. 1. 中国地质大学(北京)地球科学与资源学院, 北京 100083;
    2. 国土资源部矿产勘查技术指导中心, 北京 100034;
    3. 中国地质调查局发展研究中心, 北京 100037;
    4. 核工业北京地质研究院, 北京 100029;
    5. 成都理工大学地球科学学院, 成都 610059;
    6. 云南铜业矿产资源勘查开发有限公司, 昆明 650001;
    7. 河北省地矿局第五地质大队, 河北 唐山 063000
  • 收稿日期:2014-10-14 发布日期:2015-05-26
  • 通讯作者: 吕志成(1966),男,研究员,博士,主要从事矿床学及地球化学方面的研究工作,E-mail:zhichenglv@163.com。 E-mail:zhichenglv@163.com
  • 作者简介:姚磊(1986),男,博士研究生,主要从事矿床学及矿床地球化学研究,E-mail:lemmon20054255@aliyun.com
  • 基金资助:

    国土资源公益性行业科研专项项目(201411024);中国地质调查局老矿山找矿技术创新与示范项目(1212011220737);中国地质调查局地质调查项目(12120113090000)

Petrogenesis, Geochemistry and Zircon U-Pb Age of the Granite from No.Ⅵ Section of Hutouya Deposit, Qimantag Area, Qinghai Province, and Its Geological Significance

Yao Lei1,2, Lü Zhicheng2,3, Yu Xiaofei2,3, Pang Zhenshan2,3, Cai Yuqi4, Liu Peng5, Liu Changcheng6, Wang Fenglan7   

  1. 1. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China;
    2. Mineral Exploration Technical Guidance Center, Ministry of Land and Resources, Beijing 100034, China;
    3. Development and Research Centre, China Geological Survey, Beijing 100037, China;
    4. Beijing Research Institute of Uranium Geology, Beijing 100029, China;
    5. College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China;
    6. Yunnan Company (Ltd) of Exploration & Development of Cu Mineral Resources, Kunming 650001, China;
    7. The Fifth Geology Company of Hebei Geology and Minerals Bureau, Tangshan 063000, Hebei, China
  • Received:2014-10-14 Published:2015-05-26

PDF (PC)

572

摘要：

利用LA-ICP-MS锆石U-Pb法,测得与成矿有关的青海祁漫塔格地区虎头崖矿床Ⅵ矿带花岗岩的成岩年龄为(233.6±1.8) Ma(MSWD=1.2,n=17)。地球化学特征显示:花岗岩属高钾钙碱性、弱过铝质花岗岩;样品的稀土元素组成以总体右倾,轻、重稀土分异明显和具明显的负铕异常为特征;微量元素具有富集Rb、Th、U、La、Nd等大离子亲石元素,亏损Ba、Sr、Nb、P、Ti等元素的特点。Sr-Nd同位素组成特征显示,花岗岩的源区可能是富集岩石圈地幔。初步研究认为,虎头崖矿床Ⅵ矿带花岗岩可能形成于中、晚三叠世碰撞后碰撞的构造背景下。

关键词: 花岗岩, 锆石U-Pb年龄, Sr-Nd同位素, 虎头崖矿床, 祁漫塔格, 青海

Abstract:

Zircon LA-ICP-MS dating of the granite from the No.Ⅵ section of Hutouya deposit yields an emplacement age of (233.6±1.8) Ma (MSWD=1.2, n=17). The geochemical analysis indicates that the granite belongs to the weakly peraluminous granitic rocks, showing the nature of high-K calc-alkalic series. The rock has high REE content, and the chondrite-normalized REE distribution patterns show the characteristics of LREE enrichment, obvious LREE and HREE fractionation, and significant negative Eu anomaly. The trace element composition of the granite is enriched in Rb, Th, U, La, Nd and poor in Ba, Sr, Nb, P, Ti. The Sr-Nd isotope composition and geochemical characteristics indicate that the magma source of the granite mainly derived from enriched lithospheric mantle. The data of this study indicate that the granite from the No.Ⅵ section of Hutouya deposit formed under a collision, and post-collision setting.

Key words: granite, zircon U-Pb dating, Sr-Nd isotope composition, Hutouya deposit, Qimantag, Qinghai

中图分类号: 

  • P59

[1] 莫宣学,罗照华,邓晋福,等. 东昆仑造山带花岗岩及地壳生长[J]. 高校地质学报,2007,13(3):403-414. Mo Xuanxue, Luo Zhaohua, Deng Jinfu, et al. Granitoids and Crustal Growth in the East-Kunlun Orogenic Belt[J]. Geological Journal of China Universities, 2007, 13(3): 403-414.

[2] 毛景文,周振华,丰成友,等. 初论中国三叠纪大规模成矿作用及其动力学背景[J]. 中国地质,2012,39(6):1437-1471. Mao Jingwen, Zhou Zhenhua, Feng Chengyou, et al. A Preliminary Study of the Triassic Large-Scale Mineralization in China and Its Geodynamic Setting[J]. Geology in China, 2012, 39(6): 1437-1471.

[3] 赵一鸣,丰成友,李大新,等. 青海西部祁漫塔格地区主要矽卡岩铁多金属矿床成矿地质背景和矿化蚀变特征[J]. 矿床地质,2013,32(1):1-19. Zhao Yiming, Feng Chengyou, Li Daxin, et al. Metallogenic Setting and Mineralization-Alteration Characteristics of Major Skarn Fe-Polymetallic Deposits in Qimantag Area, Western Qinghai Province[J]. Mineral Deposits, 2013, 32(1): 1-19.

[4] 张爱奎,刘光莲,丰成友,等. 青海虎头崖多金属矿床地球化学特征及成矿-控矿因素研究[J]. 矿床地质,2013,32(1):94-108. Zhang Aikui, Liu Guanglian, Feng Chengyou, et al. Geochemical Characteristics and Ore-Controlling Factors of Hutouya Polymetallic Deposit, Qinghai Province[J]. Mineral Deposits, 2013, 32(1): 94-108.

[5] 许志琴,杨经绥,李海兵,等. 造山的高原:青藏高原的地体拼合、碰撞造山及隆升机制[M]. 北京:地质出版社,2007:1-7. Xu Zhiqin, Yang Jingsui, Li Haibing, et al. Orogenic Plateau:Terrane Amalgamation, Collision and Uplift in the Qinghai-Tibet Plateau[M]. Beijing: Geological Publishing House, 2007: 1-7.

[6] 姜春发,杨经绥,冯秉贵,等. 昆仑开合构造[M]. 北京:地质出版社,1992. Jiang Chunfa, Yang Jingsui, Feng Binggui, et al. Opening-Closing Tectonics of Kunlun Mountains[M]. Beijing: Geological Publishing House, 1992.

[7] 李世金,孙丰月,丰成友,等. 青海东昆仑鸭子沟多金属矿的成矿年代学研究[J]. 地质学报,2008,82(7):949-955. Li Shijin, Sun Fengyue, Feng Chengyou, et al. Geochronological Study on Yazigou Polymetallic Deposit in Eastern Kunlun, Qinhai Province[J]. Acta Geologica Sinica, 2008, 82(7): 949-955.

[8] 佘宏全,张德全,景向阳,等. 青海省乌兰乌珠尔斑岩铜矿床地质特征与成因[J]. 中国地质,2007,34(2):306-314. She Hongquan, Zhang Dequan, Jing Xiangyang, et al. Geological Characteristics and Genesis of the Ulan Uzhur Porphyry Copper Deposit in Qinghai[J]. Geology in China, 2007, 34(2): 306-314.

[9] 高永宝,李文渊,马晓光,等.东昆仑尕林格铁矿床成因年代学及Hf同位素制约[J]. 兰州大学学报:自然科学版,2012,48(2):36-47. Gao Yongbao, Li Wenyuan, Ma Xiaoguang, et al. Genesis, Geochronology and Hf Isotopic Compositions of the Magmatic Rocks in Galinge Iron Deposit, Eastern Kunlun[J]. Journal of Lanzhou University: Natural Science, 2012, 48(2): 36-47.

[10] 高永宝,李文渊,钱兵,等. 东昆仑野马泉铁矿相关花岗质岩体年代学、地球化学及Hf同位素特征[J]. 岩石学报,2014,30(6):1647-1665. GaoYongbao, Li Wenyuan, Qian Bing, et al. Geochronology, Geochemistry and Hf Isotopic Compositions of the Granitic Rocks Related with Iron Mineralization in Yemaquan Deposit, East Kunlun, NW China[J]. Acta Petrologica Sinica, 2014, 30(6): 1647-1665.

[11] 奚仁刚,校培喜,伍跃中,等. 东昆仑肯德可克铁矿区二长花岗岩组成、年龄及地质意义[J]. 西北地质,2010,43(4):195-202. Xi Rengang, Xiao Peixi, Wu Yuezhong, et al. The Geological Significances, Composition and Age of the Monzonitic Granite in KendekekeIron Mine[J]. Northwestern Geology, 2010, 43(4): 195-202.

[12] 吴祥珂,孟繁聪,许虹,等. 青海祁漫塔格玛兴大坂晚三叠世花岗岩年代学、地球化学及Nd-Hf同位素组成[J]. 岩石学报,2011,27(11):3380-3394. Wu Xiangke, Meng Fancong, Xu Hong, et al. Zircon U-Pb Dating, Geochemistry and Nd-Hf Isotopic Compositions of the Maxingdaban Late Triassic Granitic Pluton from Qimantag in the Eastern Kunlun[J]. Acta Geologica Sinica, 2011, 27(11): 3380-3394.

[13] 肖晔,丰成友,刘建楠,等. 青海肯德可克铁多金属矿区年代学及硫同位素特征[J]. 矿床地质,2013,32(1):177-186. Xiao Ye, Feng Chengyou, Liu Jiannan, et al. LA-MC-ICP-MS Zircon U-Pb Dating and Sulfur Isotope Characteristics of Kendekeke Fe-Polymetallic Deposit, Qinghai Province[J]. Mineral Deposits, 2013, 32(1): 177-186.

[14] 丰成友,王雪萍,舒晓峰,等.青海祁漫塔格虎头崖铅锌多金属矿区年代学研究及地质意义[J]. 吉林大学学报:地球科学版,2011,41(6):1806-1817. Feng Chengyou, Wang Xueping, Shu Xiaofeng, et al. Isotopic Chronology of the Hutouya Skarn Lead-Zinc Polymetallic Ore District in Qimantage Area of Qinghai Province and Its Geological Significance[J]. Journal of Jilin University: Earth Science Edition, 2011, 41(6): 1806-1817.

[15] 丰成友,王松,李国臣,等. 青海祁漫塔格中晚三叠世花岗岩:年代学、地球化学及成矿意义[J]. 岩石学报,2012,28(2):665-678. Feng Chengyou, Wang Song, Li Guochen, et al. Middle to Late Triassic Granitoids in the Qimantage Area, Qinghai Province, China: Chronology, Geochemistry and Metallogenic Significances[J]. Acta Petrologic Sinica, 2012, 28(2): 665-678.

[16] 王松,丰成友,李世金,等. 青海祁漫塔格卡尔却卡铜多金属矿区花岗闪长岩锆石SHRIMPU-Pb测年及其地质意[J]. 中国地质,2009,36(1):74-84. Wang Song, Feng Chengyou, Li Shijin, et al. Zircon SHRIMP U-Pb Dating of Granodiorite in the Kaerqueka Polymetallic Ore Deposit, Qimantage Mountain, Qinghai Province, and Its Geological Implications[J]. Geology in China, 2009, 36(1): 74-84.

[17] 陈静,谢智勇,李彬,等. 东昆仑拉陵灶火钼多金属矿床含矿岩体地质地球化学特征及其成矿意义[J]. 地质与勘探,2013,49(5):813-824. Chen Jing, Xie Zhiyong, Li Bin, et al. Geological and Gechemical Characteristics of the Ore-Bearing Intrusions from the Lalingzaohuo Mo Polymetallic Deposit and Its Metallogenic Significance[J]. Geology and Exploration, 2013, 49(5): 813-824.

[18] 许庆林,孙丰月,李碧乐,等. 东昆仑莫河下拉银多金属矿床花岗斑岩年代学、地球化学特征及其构造背景[J]. 大地构造与成矿学,2014,38(2):421-433. Xu Qinglin, Sun Fengyue, Li Bile, et al. Geochronological Dating, Geochemical Characteristics and TectonicSetting of the Granite-Porphyry in the Mohexiala Silver Polymetallic Deposit, Eastern Kunlun Orogenic Belt[J]. Geotectonicaet Metallogenia, 2014, 38(2): 421-433.

[19] 青海地质矿产局. 青海省区域地质志[M]. 北京:地质出版社,1991. Bureau of Geology and Mineral Resources of Qinghai Province. Regional Geology of Qinghai Province[M]. Beijing: Geological Publishing House, 1991.

[20] 于淼,丰成友,保广英,等. 青海尕林格铁矿床矽卡岩矿物学及蚀变分带[J]. 矿床地质,2013,32(1):55-76. Yu Miao, Feng Chengyou, Bao Guangying, et al. Characteristics and Zonation of Skarn Minerals in GalingeIron Deposit, Qinghai Province[J]. Mineral Deposits, 2013, 32(1): 55-76.

[21] 胡永达,孙丰月,李碧乐,等. 青海东昆仑乌兰乌珠尔铜矿金属矿物特征及意义[J]. 地质与资源,2006,15(3):191-199. Hu Yongda, Sun Fengyue, Li Bile, et al. Characteristics and Significance of Metallic Minerals from Wulanwuzhuer Copper Deposit in the Eastern Kunlun Orogenic Belt, Qinghai Province[J]. Geology and Resources, 2006, 15(3): 191-199.

[22] 何书跃,李东生,李良林,等. 青海东昆仑鸭子沟斑岩型铜(钼)矿区辉钼矿铼-锇同位素年龄及地质意义[J]. 大地构造与成矿学,2009,33(2):236-242. He Shuyue, Li Dongsheng, Li Lianglin, et al. Re-Os Age of Molybdenite from the Yazigou Copper (Molybdenum) Mineralized Area in Eastern Kunlun of Qinghai Province, and Its Geological Significance[J]. Geotectonicaet Metallogenia, 2009, 33(2): 236-242.

[23] 刘渭,杨兴科,王守良,等. 青海省祁漫塔格矿带虎头崖矿田构造控矿特征[J]. 中国地质,2014,41(1):222-234. Liu Wei, Yang Xingke, Wang Shouliang, et al. Characteristics of Ore-Controlling Structures of the Hutouya Orefieldin the Qimantage Metallogenic Belt, Qinghai Province[J]. Geology in China, 2014,41(1): 222-234.

[24] 侯可军,李延河,田有荣. LA-MC-ICP-MS锆石微区原位U-Pb定年技术[J]. 矿床地质,2009,28(4):481-492. Hou Kejun, Li Yanhe, TianYourong. In Situ U-Pb Zircon Dating Using Laser Ablation-Multiion Conting LA-MC-ICP-MS[J]. Mineral Deposits, 2009, 28 (4): 481-492.

[25] 赵海杰,毛景文,向君峰,等.湖北铜绿山矿床石英闪长岩的矿物学及Sr-Nd-Pb同位素特征[J]. 岩石学报,2010,26(3):768-784. Zhao Haijie, Mao Jingwen, Xiang Junfeng, et al. Mineralogy and Sr-Nd-Pb Isotopic Compositions of Quartz Diorite in Tonglushan Deposit, Hubei Province[J]. Acta Petrologica Sinica, 2010, 26 (3): 768-784.

[26] Hoskin P W O, Black L P. Metamorphic Zircon Formation by Solid-State Recrystallization of Protolith Igneous Zircon[J]. Journal of Metamorphic Geology, 2000, 18: 423-439.

[27] Middlemost E A. Naming Materials in the Magma/Igneous Rock System[J]. Earth Science Review, 1994, 37: 215-224.

[28] Le Maitre R W. Igneous Rocks: A Classification and Glossary of Terms[M]. 2nd Edition. Cambridge: Cambridge Univercity Press, 2002: 236.

[29] Maniar P D, Piccoli P M. Tectonic Discrimination of Granitoids[J]. Geological Society of America Bulletin, 1989, 101: 635-643.

[30] Boynton W V. Cosmochemistry of the Rare Earth Elements: Meteorite Studies[M]//Henderson P. Rare Earth Element Geochemistry.Amsterdam: Elsevier, 1984: 63-114.

[31] McDonough W F, Sun S S. The Composition of the Earth[J]. Chemical Geology, 1995, 120: 223-235.

[32] Whalen J, Currie K, Chappell B. A-Type Granites: Geochemical Characteristics, Discrimination and Petrogenesis[J]. Contributions to Mineralogy and Petrology, 1987, 95:407-419.

[33] 余能,金巍,葛文春,等. 东昆仑金水口过铝花岗岩的地球化学研究[J]. 世界地质,2005,24(2):123-128. Yu Neng, Jin Wei, Ge Wenjun, et al. Geochemical Study on Peraluminous Granite from Jinshuikou in East Kunlun[J]. Global Geology, 2005, 24(2): 123-128.

[34] 刘成东,莫宣学,罗照华,等. 东昆仑造山带花岗岩类Pb-Sr-Nd-O同位素特征[J]. 地球学报,2003,24(6):584-588. Liu Chengdong, Mo Xuanxue, Luo Zhaohua, et al. Pb-Sr-Nd-O Isotope Characteristics of Granitoids in East Kunlun Orogenic Belt[J]. Acta Geoscientica Sinica, 2003, 24(6): 584-588.

[35] 邓晋福,吴宗絮,杨建军,等. 格尔木额济纳旗地学断面走廊域地壳-上地幔岩石学结构与深部过程[J]. 地球物理学报,1995,38,(增刊Ⅱ):130-144. Deng Jinfu, Wu Zongxu, Yang Jianjun, et al. Crust-Mantle Petrological Structure and Deep Processes Along the Golmud-Ejinqi Geoscience Section[J]. Acta Geophysica Sinica, 38 (Sup.II): 130-144.

[36] 熊富浩,马昌前,张金阳,等. 东昆仑造山带早中生代镁铁质岩墙群LA-ICP-MS锆石U-Pb定年、元素和Sr-Nd-Hf同位素地球化学[J]. 岩石学报,2011,27(11):3350-3364. Xiong Fuhao, Ma Changqian, Zhang Jinyang, et al. LA-ICP-MS Zircon U-Pb Dating, Elements and Sr-Nd-Hf Isotope Geochemistry of the Early Mesozoic Mafic Dyke Swarms in East Kunlun Orogenic Belt[J].Acta Petrologica Sinica, 2011, 27(11): 3350-3364.

[37] Zhang J Y, Ma C Q, Xiong F H, et al. Petrogenesis and Tectonic Significance ofthe Late Permian-Middle Triassic Calc-Alkaline Granites in the Balong Region, Eastern Kunlun Orogen, China[J]. Geological Magazine, 2012, 149:892-908.

[38] 谌宏伟,罗照华,莫宣学,等. 东昆仑造山带三叠纪岩浆混合成因花岗岩的岩浆底侵作用机制[J]. 中国地质,2005,32(3):386-395. Chen Hongwei, Luo Zhaohua, Mo Xuanxue, et al. Underplating Mechanism of Triassic Granite of Magma Mixing Origin in the East Kunlun Orogenic Belt[J]. Geology in China, 32(3): 386-395.

[39] 王冠,孙丰月,李碧乐,等. 东昆仑夏日哈木矿区闪长岩锆石U-Pb年代学、地球化学及其地质意义[J]. 吉林大学学报:地球科学版,2014,44(3):876-891. Wang Guan, Sun Fengyue, Li Bile, et al. Zircon U-Pb Geochronology and Geochemistry of Diorite in Xiarihamu Ore District from East Kunlun and Its Geological Significance[J]. Journal of Jilin University: Earth Science Edition, 2014, 44(3): 876-891.

[40] 郭正府,邓晋福,许志琴,等. 青藏东昆仑晚古生代末中生代中酸性火成岩与陆内造山过程[J]. 现代地质,1998,12(3):344-352. Guo Zhengfu, Deng Jinfu, Xu Zhiqin, et al. Late Palaeozoic-Mesozoic Intracontinental Orogenic Process and Intermediate-Acidic Igneous Rocks from the Eastern Kunlun Mountains of Northwestern China[J]. Geoscience, 1998, 12(3): 344-352.

[41] Pearce J A, Harris N B W, Tindle A G. Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks[J]. Journal of Petrology,1984, 25: 956-983.

[42] Pearce J A. Sources and Settings of Granitic Rocks[J]. Episodes, 1996, 6: 120-125.
[1] 高飞, 刘永江, 温泉波, 李伟民, 冯志强, 范文亮, 汤超. 内蒙古突泉—科尔沁右翼中旗地区中生代花岗岩锆石U-Pb年龄及其地质意义[J]. 吉林大学学报(地球科学版), 2018, 48(3): 769-783.
[2] 尹业长, 郝立波, 赵玉岩, 石厚礼, 田午, 张豫华, 陆继龙. 冀东高家店和蛇盘兔花岗岩体:年代学、地球化学及地质意义[J]. 吉林大学学报(地球科学版), 2018, 48(2): 574-586.
[3] 齐天骄, 薛春纪, 许碧霞. 新疆昭苏布合塔铜(金)矿化区花岗质岩石锆石U-Pb年龄、地球化学特征及其成因[J]. 吉林大学学报(地球科学版), 2018, 48(1): 132-144.
[4] 高红梅, 兰永伟, 周莉, 孟丽岩. 温度作用下缺陷花岗岩热损伤:以甘肃北山缺陷花岗岩为例[J]. 吉林大学学报(地球科学版), 2017, 47(6): 1795-1802.
[5] 杨凤超, 宋运红, 赵玉岩. 辽宁盘岭矿集区花岗岩锆石SHRIMP U-Pb年龄、Hf同位素组成及地质意义[J]. 吉林大学学报(地球科学版), 2017, 47(5): 1429-1441.
[6] 赵院冬, 车继英, 吴大天, 许逢明, 赵君, 李士超. 小兴安岭西北部早—中侏罗世TTG花岗岩年代学、地球化学特征及构造意义[J]. 吉林大学学报(地球科学版), 2017, 47(4): 1119-1137.
[7] 郗爱华, 王明智, 葛玉辉, 李碧乐, 王泉, 朱靓. 黑龙江省五道岭地区花岗斑岩地球化学特征及地质意义[J]. 吉林大学学报(地球科学版), 2017, 47(4): 1159-1171.
[8] 叶霖, 刘玉平, 张乾, 鲍谈, 何芳, 王小娟, 王大鹏, 蓝江波. 云南都龙超大型锡锌多金属矿床中闪锌矿微量及稀土元素地球化学特征[J]. 吉林大学学报(地球科学版), 2017, 47(3): 734-750.
[9] 孙珍军, 孙国胜, 于赫楠, 向柱, 田毅, 刘彤, 陈旭, 李杨. 赤峰撰山子花岗岩年代学、地球化学特征及其成岩动力学背景[J]. 吉林大学学报(地球科学版), 2016, 46(6): 1740-1753.
[10] 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.
[11] 张雨晴, 王晖, 范廷恩, 宋来明, 聂妍, 梁旭, 陈飞. 花岗岩潜山储层裂缝建模表征方法——以渤海花岗岩潜山A油田为例[J]. 吉林大学学报(地球科学版), 2016, 46(5): 1312-1320.
[12] 郭宇飞, 杨言辰, 韩世炯, 谈艳, 薄军委. 大兴安岭北部凤凰山地区英云闪长岩地球化学特征与锆石U-Pb定年[J]. 吉林大学学报(地球科学版), 2016, 46(5): 1406-1417.
[13] 李剑波, 王保宏, 杨亮, 景耀祖, 陈利珍. 内蒙古乌拉特中旗德岭山地区石英闪长岩的锆石U-Pb年龄及地质意义[J]. 吉林大学学报(地球科学版), 2016, 46(5): 1430-1439.
[14] 王科强, 张德会, 朱玉娣, 付芬, 印贤波, 王晨昇. 浙江常山里山岭斑岩型铜矿床成岩时代及岩浆源区[J]. 吉林大学学报(地球科学版), 2016, 46(3): 736-748.
[15] 张晓飞, 李智明, 贾群子, 宋忠宝, 陈向阳, 张雨莲, 李东生, 舒晓峰. 青海祁漫塔格虎头崖多金属矿区花岗斑岩地球化学、年代学特征及其地质意义[J]. 吉林大学学报(地球科学版), 2016, 46(3): 749-765.
Viewed
Full text
372
HTML PDF
Just accepted Online first Issue Just accepted Online first Issue
0 0 0 0 0 372

  From Others local
  Times 117 255
  Rate 31% 69%

Abstract
516
Just accepted Online first Issue
0 0 516
  From Others local
  Times 429 87
  Rate 83% 17%

Cited
Web of Science  Crossref   ScienceDirect  Search for Citations in Google Scholar >>
 
This page requires you have already subscribed to WoS.
  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