Institute of Geomechanics, Chinese Academy of Geological SciencesHost
Advanced Search
Previous Article Next Article
2018 Vol. 24, No. 3
Article Contents
Article navigation > Journal of Geomechanics > 2018 > 24(3): 341-349
Next Article Previous Article

Yangyang HE, Chunqi WEN, Xianfan LIU. GEOCHEMICAL CHARACTERISTICS OF GRANODIORITE PORPHYRY AND MINERALIZATION STUDY IN THE GAERQIN COPPER DEPOSIT, TIBET[J]. Journal of Geomechanics, 2018, 24(3): 341-349. doi: 10.12090/j.issn.1006-6616.2018.24.03.036
Citation: Yangyang HE, Chunqi WEN, Xianfan LIU. GEOCHEMICAL CHARACTERISTICS OF GRANODIORITE PORPHYRY AND MINERALIZATION STUDY IN THE GAERQIN COPPER DEPOSIT, TIBET[J]. Journal of Geomechanics, 2018, 24(3): 341-349. doi: 10.12090/j.issn.1006-6616.2018.24.03.036
shu

GEOCHEMICAL CHARACTERISTICS OF GRANODIORITE PORPHYRY AND MINERALIZATION STUDY IN THE GAERQIN COPPER DEPOSIT, TIBET

  • 1.

    School of Geography and Resource Science, Neijiang Normal University, Neijiang 641112, Sichuan, China

  • 2.

    Geosciences College of Chengdu University of Technology, Chengdu 610059, Sichuan, China

More Information
Received Date:  09 July 2017
Revised Date:  20 May 2018
    Abstract
  • The rare earth elements (REEs) in granodiorite porphyry and zircon from the Gaerqin copper deposit of Tibet, China, were geochemically traced, and the mineralization was also studied. The total levels of REEs in granodiorite porphyry varied slightly (ΣREE=48.64×10-6~78.12×10-6) with LREE/HREE=8.67~11.68. All samples were featured by a right-leaning distribution with enrichment in light REEs (LREEs) and depletion in heavy REEs (HREEs), δEu changed from weak negative anomaly to weak positive anomaly, which is due to the gradual weakening of negative Eu anomalies caused by crystallization differentiation and a weak positive Eu anomaly in the process of the partially remelting growth of the angled magma in the crust. The zircon was found with typical oscillatory zones, large total REE levels (ΣREE=735.78×10-6~6792.10×10-6), LREE depletion, HREE enrichment, evident Ce positive anomaly and weak negative Eu anomaly. This is because under the action of mantle fluid, heavy rare earth elements and Ce are more likely to enter the lattice of zircon than other light rare-earth elements. The weak negative abnormality of Eu is caused by oxidation and leaching of the late diagenetic rock mass. Comprehensive analysis reveals that the mantle fluid action endowed the granodiorite porphyry with the characteristics of crust-mantle mixing or even ore-formation. Meanwhile, the matter-energy exchange between magma and surrounding rocks accounted for the metamorphic sandstone ore-formation.
    • FullText(HTML)
  • 加载中
    • References
  • 吴福元, 李献华, 郑永飞, 等. Lu-Hf同位素体系及其岩石学应用[J].岩石学报, 2007, 23(2):185~220.

    Google Scholar

    WU Fuyuan, LI Xianhua, ZHENG Yongfei, et al. Lu-Hf isotopic systematics and their applications in petrology[J]. Acta Petrologica Sinica, 2007, 23(2):185~220. (in Chinese with English abstract)

    Google Scholar

    雷玮琰, 施光海, 刘迎新.不同成因锆石的微量元素特征研究进展[J].地学前缘, 2013, 20(4):273~284.

    Google Scholar

    LEI Weiyan, SHI Guanghai, LIU Yingxin. Research progress on trace element characteristics of zircons of different origins[J]. Earth Science Frontiers, 2013, 20(4):273~284. (in Chinese with English abstract)

    Google Scholar

    Zhang H, Yuan H L, Hu Z C, et al. Characteristics of rare earth elements of zircons from Mesozoic volcanic rocks in Luanping region, Hebei[J]. Journal of Rare Earths, 2005, 23(5):588~595.

    Google Scholar

    曹烨, 李胜荣, 李真真, 等.太行山北段石湖金矿区中生代岩浆岩中单颗粒锆石的稀土元素特征及启示[J].中国稀土学报, 2009, 27(4):564~573.

    Google Scholar

    CAO Ye, LI Shengrong, LI Zhenzhen, et al. Characteristics of rare earth elements of zircon from Mesozoic magmatic rocks in Shihu gold district, north Taihang mountain, north China[J]. Journal of the Chinese Rare Earth Society, 2009, 27(4):564~573. (in Chinese with English abstract)

    Google Scholar

    王亚伟, 刘良, 廖小莹, 等.秦岭杂岩清油河斜长角闪岩多期变质的证据——来自锆石微量元素和包裹体的启示[J].岩石学报, 2016, 32(5):1467~1492.

    Google Scholar

    WANG Yawei, LIU Liang, LIAO Xiaoying, et al. Multi-metamorphism of amphibolite in the Qinling complex, Qingyouhe area:Revelation from trace elements and mineral inclusions in zircons[J]. Acta Petrologica Sinica, 2016, 32(5):1467~1492. (in Chinese with English abstract)

    Google Scholar

    方向, 丁帅, 王艺云, 等.西藏多龙矿集区尕尔勤铜金矿区成矿潜力预测[J].矿床地质, 2014, 33(S1):1005~1006.

    Google Scholar

    FANG Xiang, DING Shuai, WANG Yiyun, et al. Prediction of metallogenic potential in the Gaerqin copper-gold deposit in the Duolong Ore Concentration Area, Tibet[J]. Mineral Deposits, 2014, 33(S1):1005~1006. (in Chinese with English abstract)

    Google Scholar

    林彬, 唐菊兴, 宋扬, 等.藏北多龙矿集区尕尔勤枕状玄武岩地球化学及SHRIMP测年[J].地球学报, 2017, 38(5):702~710. doi: 10.3975/cagsb.2017.05.10

    CrossRef Google Scholar

    LIN Bin, TANG Juxing, SONG Yang, et al. Petrogeochemistry and SHRIMP dating of Ga'erqin pillow basalt in Duolong, northern Tibet[J]. Acta Geoscientica Sinica, 2017, 38(5):702~710. (in Chinese with English abstract) doi: 10.3975/cagsb.2017.05.10

    CrossRef Google Scholar

    张志, 方向, 唐菊兴, 等.西藏多龙矿集区尕尔勤斑岩铜矿床年代学及地球化学——兼论硅帽的识别与可能的浅成低温热液矿床[J].岩石学报, 2017, 33(2):476~494.

    Google Scholar

    ZHANG Zhi, FANG Xiang, TANG Juxing, et al. Chronology, geochemical characteristics of the Gaerqin porphyry copper deposit in the Duolong ore concentration area in Tibet and discussion about the identification of the lithoscaps and the possible epithermal deposit[J]. Acta Petrologica Sinica, 2017, 33(2):476~494. (in Chinese with English abstract)

    Google Scholar

    祝向平, 陈华安, 马东方, 等.西藏多不杂斑岩铜金矿床地质与蚀变[J].地质与勘探, 2012, 48(2):199~206.

    Google Scholar

    ZHU Xiangping, CHEN Huaan, MA Dongfang, et al. Geology and alteration of the Duobuza porphyry copper-gold deposit in Tibet[J]. Geology and Exploration, 2012, 48(2):199~206. (in Chinese with English abstract)

    Google Scholar

    何阳阳, 温春齐, 刘显凡, 等.西藏多不杂铜矿区曲色组砂岩化学组分特征及构造背景[J].成都理工大学学报(自然科学版), 2014, 41(1):113~118.

    Google Scholar

    HE Yangyang, WEN Chunqi, LIU Xianfan, et al. Chemical component characteristics and tectonic setting of sandstone from quse group in Duobuza copper deposit, Tibet, China[J]. Journal of Chengdu University of Technology (Science & Technology Edition), 2014, 41(1):113~118. (in Chinese with English abstract)

    Google Scholar

    Hou Z Q, Gao Y F, Qu X M, et al. Origin of adakitic intrusives generated during mid-Miocene East-west extension in southern Tibet[J]. Earth and Planetary Science Letters, 2004, 220:139~155. doi: 10.1016/S0012-821X(04)00007-X

    CrossRef Google Scholar

    陈红旗, 张天平, 李玉昌, 等. 西藏班公湖-怒江成矿带西段铜多金属资源调查报告[R]. 拉萨: 西藏自治区地质调查院, 2011.

    Google Scholar

    CHEN Hong-qi, ZHANG Tian-ping, LI Yu-chang, et al. Resources investigation report of Copper polymetallic in the Western Bangonghu-Nujiang Metallogenic Belt, Tibet[R]. Lhasa: Geological Survey of Tibet Autonomous Region, 2011. (in Chinese)

    Google Scholar

    Belousova E A, Griffin W L, O'Reilly S Y. Zircon crystal morphology, trace element signatures and Hf isotope composition as a tool for petrogenetic modelling:examples from eastern Australian granitoids[J]. Journal of Petrology, 2006, 47(2):329~353. doi: 10.1093/petrology/egi077

    CrossRef Google Scholar

    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.http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kxtb200416002

    Google Scholar

    Hoskin P W O, Schaltegger U. The composition of zircon and igneous and metamorphic petrogenesis[J]. Reviews in Mineralogy and Geochemistry, 2003, 53(1):27~62. doi: 10.2113/0530027

    CrossRef Google Scholar

    Boynton W V. Cosmochemistry of the rare earth elements:meteorite studies[J]. Developments in Geochemistry, 1984, 2:63~114. doi: 10.1016/B978-0-444-42148-7.50008-3

    CrossRef Google Scholar

    何阳阳, 温春齐, 刘显凡.西藏多不杂铜矿床稀土元素地球化学特征研究[J].中国稀土学报, 2018, 36(1):122~128.

    Google Scholar

    HE Yangyang, WEN Chunqi, LIU Xianfan. REE Geochemical characteristics of the Duobuza copper deposit, Tibet[J]. Journal of the Chinese Society of Rare Earths, 2018, 36(1):122~128. (in Chinese with English abstract)

    Google Scholar

    刘显凡, 楚亚婷, 卢秋霞, 等.云南老王寨金矿的深部地质过程——来自显微岩相学和元素地球化学的证据[J].吉林大学学报(地球科学版), 2012, 42(4):1026~1038.

    Google Scholar

    LIU Xianfan, CHU Yating, LU Qiuxia, et al. Deep geological processes on Laowangzhai gold deposit in Yunnan:evidence from petrography and element geochemistry[J]. Journal of Jilin University (Earth Science Edition), 2012, 42(4):1026~1038. (in Chinese with English abstract)

    Google Scholar

    Liu X F, Li C H, Lu Q X, et al. The genesis mechanism of the mantle fluid action and evolution in the ore-forming process:a case study of the Laowangzhai gold deposit in Yunnan, China[J]. Acta Geologica Sinica (English Edition), 2012, 86(3):608~618. doi: 10.1111/acgs.2012.86.issue-3

    CrossRef Google Scholar

    李春辉, 刘显凡, 赵甫峰, 等.金顶超大型铅锌矿床中的地幔流体现实踪迹与壳幔混染叠加成矿机制[J].地学前缘, 2011, 18(1):194~206.

    Google Scholar

    LI Chunhui, LIU Xianfan, ZHAO Fufeng, et al. Actual traces of mantle fluid of Jinding super-large Pb-Zn deposit and the mechanism of crust-mantle overlapping mineralization[J]. Earth Science Frontiers, 2011, 18(1):194~206. (in Chinese with English abstract)

    Google Scholar

    邓碧平, 刘显凡, 朱建军, 等.壳幔混染成矿机制的稀有气体同位素及硅同位素证据以滇西富碱斑岩型多金属矿区为例[J].吉林大学学报(地球科学版), 2014, 44(6):1856~1868.

    Google Scholar

    DENG Biping, LIU Xianfan, ZHU Jianjun, et al. Noble gas isotope and silicon isotope evidences of crust-mantle mixing ore-formation mechanism:examplified by the alkali-rich porphyry polymetallic deposits in western Yunnan, China[J]. Journal of Jilin University (Earth Science Edition), 2014, 44(6):1856~1868. (in Chinese with English abstract)

    Google Scholar

    王金荣, 陈万峰, 张旗, 等. N-MORB和E-MORB数据挖掘——玄武岩判别图及洋中脊源区地幔性质的讨论[J].岩石学报, 2017, 33(3):993~1005.

    Google Scholar

    WANG Jinrong, CHEN WanFeng, ZHANG Qi, et al. Preliminary research on data mining of N-MORB and E-MORB:Discussion on method of the basalt discrimination diagrams and the character of MORB's mantle source[J]. Acta Petrologica Sinica, 2017, 33(3):993~1005. (in Chinese with English abstract)

    Google Scholar

    张旗, 王焰, 钱青, 等.中国东部燕山期埃达克岩的特征及其构造-成矿意义[J].岩石学报, 2001, 17(2):236~244.

    Google Scholar

    ZHANG Qi, WANG Yan, QIAN Qing, et al. The characteristics and tectonic-metallogenic significances of the adakites in Yanshan period from eastern China[J]. Acta Petrologica Sinica, 2001, 17(2):236~244. (in Chinese with English abstract)

    Google Scholar

    佘宏全, 李进文, 马东方, 等.西藏多不杂斑岩铜矿床辉钼矿Re-Os和锆石U-Pb SHRIMP测年及地质意义[J].矿床地质, 2009, 28(6):737~746.

    Google Scholar

    SHE Hongquan, LI Jinwen, MA Dongfang, et al. Molybdenite Re-Os and SHRIMP zircon U-Pb dating of Duobuza porphyry copper deposit in Tibet and its geological implications[J]. Mineral Deposits, 2009, 28(6):737~746. (in Chinese with English abstract)

    Google Scholar

    Zhou X, Fei G C, Zhou Y, et al. Chronology and crust-mantle mixing of ore-forming porphyry of the bangongco:evidence from zircon U-Pb age and Hf isotopes of the naruo porphyry copper-gold deposit[J]. Acta Geologica Sinica (English Edition), 2015, 89(1):217~228. doi: 10.1111/1755-6724.12406

    CrossRef Google Scholar

    Fei G C, Zhou X, Duo J, et al. Zircon U-Pb age and geochemical characteristics of ore-bearing granodiorite porphyry in the Duobuza porphyry copper deposit, Tibet[J]. Journal of the Geological Society of India, 2015, 86(2):223~232. doi: 10.1007/s12594-015-0302-8

    CrossRef Google Scholar

    符家骏, 赵元艺, 郭硕.西藏多龙矿集区花岗闪长斑岩地球化学特征及其意义[J].岩石矿物学杂志, 2014, 33(6):1039~1051.

    Google Scholar

    FU Jiajun, ZHAO Yuanyi, GUO Shuo. Geochemical characteristics and significance of granodiorite porphyry in the Duolong ore concentration area, Tibet[J]. Acta Petrologica et Mineralogica, 2014, 33(6):1039~1051. (in Chinese with English abstract)

    Google Scholar

    乔东海, 赵元艺, 汪傲, 等.西藏多龙矿集区地堡铜(金)矿床年代学、流体包裹体、地球化学特征及其成因类型研究[J].地质学报, 2017, 91(7):1542~1564.

    Google Scholar

    QIAO Donghai, ZHAO Yuanyi, WANG Ao, et al. Geochronology, fluid inclusions, geochemical characteristics of Dibao Cu (Au) Deposit, Duolong ore concentration area, Xizang (Tibet), and its genetic type[J]. Acta Geologica Sinica, 2017, 91(7):1542~1564. (in Chinese with English abstract)

    Google Scholar

    王松, 赵元艺, 汪傲, 等.西藏拿顿铜(金)矿床岩矿相学、流体包裹体和地球化学特征与成矿作用研究[J].地质学报, 2017, 91(7):1565~1588.

    Google Scholar

    WANG Song, ZHAO Yuanyi, WANG Ao, et al. The study of facieology-mineragraphy, fluid inclusions, and geochemical characteristics and mineralization in Nadun Cu (Au) deposit, Tibet[J]. Acta Geologica Sinica, 2017, 91(7):1565~1588. (in Chinese with English abstract)

    Google Scholar

    何阳阳. 西藏班怒西段多不杂铜矿床成因研究[D]. 成都: 成都理工大学, 2015.http://cdmd.cnki.com.cn/Article/CDMD-10616-1015312818.htm

    Google Scholar

    HE Yangyang. Genisis study for the Duobuza copper deposit in the western part of Bangonghu-Nujiang metallogenic belt, Tibet[D]. Chengdu: Chengdu University of Technology, 2015. (in Chinese with English abstract)

    Google Scholar

    何阳阳, 温春齐, 刘显凡.西藏多不杂铜矿床硫铅同位素地球化学示踪[J].岩石矿物学杂志, 2016, 35(5):855~862.

    Google Scholar

    HE Yangyang, WEN Chunqi, LIU Xianfan. Sulfur and lead isotope geochemical tracing of the Duobuza copper deposit, Tibet[J]. Acta Petrologica et Mineralogica, 2016, 35(5):855~862. (in Chinese with English abstract)

    Google Scholar

    罗照华, 莫宣学, 卢欣祥, 等.透岩浆流体成矿作用——理论分析与野外证据[J].地学前缘, 2007, 14(3):165~183.

    Google Scholar

    LUO Zhaohua, MO Xuanxue, LU Xinxiang, et al. Metallogeny by trans-magmatic fluids-theoretical analysis and field evidence[J]. Earth Science Frontiers, 2007, 14(3):165~183. (in Chinese with English abstract)

    Google Scholar

    罗照华, 卢欣祥, 郭少丰, 等.透岩浆流体成矿体系[J].岩石学报, 2008, 24(12):2669~2678.

    Google Scholar

    LUO Zhaohua, LU Xinxiang, GUO Shaofeng, et al. Metallogenic systems on the transmagmatic fluid theory[J]. Acta Petrologica Sinica, 2008, 24(12):2669~2678. (in Chinese with English abstract)

    Google Scholar

    刘显凡, 蔡永文, 卢秋霞, 等.滇西地区富碱斑岩中地幔流体作用踪迹及其成矿作用意义[J].地学前缘, 2010, 17(1):114~136.

    Google Scholar

    LIU Xianfan, CAI Yongwen, LU Qiuxia, et al. Actual traces of mantle fluid from alkali-rich porphyries in western Yunnan, and associated implications to metallogenesis[J]. Earth Science Frontiers, 2010, 17(1):114~136. (in Chinese with English abstract)

    Google Scholar

    姜耀辉, 蒋少涌, 凌洪飞.地幔流体与铀成矿作用[J].地学前缘, 2004, 11(2):491~499.

    Google Scholar

    JIANG Yaohui, JIANG Shaoyong, LING Hongfei. Mantle-derived fluids and uranium mineralization[J]. Earth Science Frontiers, 2004, 11(2):491~499. (in Chinese with English abstract)

    Google Scholar

    杜德道, 曲晓明, 王根厚, 等.西藏班公湖-怒江缝合带西段中特提斯洋盆的双向俯冲:来自岛弧型花岗岩锆石U-Pb年龄和元素地球化学的证据[J].岩石学报, 2011, 27(7):1993~2002.

    Google Scholar

    DU Dedao, QU Xiaoming, WANG Genhou, et al. Bidirectional subduction of the Middle Tethys oceanic basin in the west segment of Bangonghu-Nujiang suture, Tibet:Evidence from zircon U-Pb LAICPMS dating and petrogeochemistry of arc granites[J]. Acta Petrologica Sinica, 2011, 27(7):1993~2002. (in Chinese with English abstract)

    Google Scholar

    • Relative Articles
  • Cited by
  • Supplements
    • Proportional views
  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Figures(5)

Tables(3)

Export Citation
PDF
XML

Article Metrics

Article views(2477) PDF downloads(74) Cited by(0)

Access History

Other Articles By Authors

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    版权所有：中国地质调查局发展研究中心 copyright @2020