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西藏尕尔勤铜矿床花岗闪长斑岩地球化学特征及成矿作用研究

何阳阳 温春齐 刘显凡

何阳阳, 温春齐, 刘显凡, 2018. 西藏尕尔勤铜矿床花岗闪长斑岩地球化学特征及成矿作用研究. 地质力学学报, 24 (3): 341-349. DOI: 10.12090/j.issn.1006-6616.2018.24.03.036
引用本文: 何阳阳, 温春齐, 刘显凡, 2018. 西藏尕尔勤铜矿床花岗闪长斑岩地球化学特征及成矿作用研究. 地质力学学报, 24 (3): 341-349. DOI: 10.12090/j.issn.1006-6616.2018.24.03.036
HE Yangyang, WEN Chunqi, LIU Xianfan, 2018. GEOCHEMICAL CHARACTERISTICS OF GRANODIORITE PORPHYRY AND MINERALIZATION STUDY IN THE GAERQIN COPPER DEPOSIT, TIBET. Journal of Geomechanics, 24 (3): 341-349. DOI: 10.12090/j.issn.1006-6616.2018.24.03.036
Citation: HE Yangyang, WEN Chunqi, LIU Xianfan, 2018. GEOCHEMICAL CHARACTERISTICS OF GRANODIORITE PORPHYRY AND MINERALIZATION STUDY IN THE GAERQIN COPPER DEPOSIT, TIBET. Journal of Geomechanics, 24 (3): 341-349. DOI: 10.12090/j.issn.1006-6616.2018.24.03.036

西藏尕尔勤铜矿床花岗闪长斑岩地球化学特征及成矿作用研究

doi: 10.12090/j.issn.1006-6616.2018.24.03.036
基金项目: 

国土资源部公益性行业科研专项项目 201011013

四川省教育厅科研项目 17ZB0223

详细信息
    作者简介:

    何阳阳(1984-), 男, 博士, 主要从事矿床学及区域成矿学研究工作。E-mail:yangyang.he@qq.com

    通讯作者:

    温春齐(1945-), 男, 教授, 主要从事矿床学及区域成矿学研究工作。E-mail:wcq@cdut.edu.cn

  • 中图分类号: P588.121;P618

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

  • 摘要: 对尕尔勤铜矿床花岗闪长斑岩及其锆石的稀土元素进行了分析,并对其成矿作用进行了研究。结果表明,花岗闪长斑岩稀土元素总含量变化范围不大(ΣREE=48.64×10-6~78.12×10-6),LREE/HREE=8.67~11.68,所有样品都呈轻稀土元素相对富集、重稀土元素亏损的右倾型分配模式;δEu由弱负异常→弱正异常演化,这是因为地幔底辟作用引发地壳部分重熔形成长英质岩浆的过程中,逐步消弱了结晶分异导致的负Eu异常进而出现弱的正Eu异常。锆石具有典型的振荡环带,稀土总量较高(ΣREE=735.78×10-6~6792.10×10-6),相对亏损轻稀土,富集重稀土,正Ce异常明显,并呈现弱的负Eu异常,这是因为在地幔流体作用下,重稀土元素及Ce较其它轻稀土元素更容易进入锆石晶格所致,Eu呈弱的负异常则是成岩后期岩体受氧化淋滤所致。综合分析,揭示出地幔流体作用导致花岗闪长斑岩具有壳幔混染甚至成矿特征,同时还能透过岩浆与围岩发生物质和能量的交换,导致变质砂岩成矿的成因机制。

     

  • 图  1  尕尔勤铜矿床大地构造位置及矿体平面图

    Figure  1.  Geotectonic location and ore body plan of the Gaerqin porphyry copper deposit

    图  2  花岗闪长斑岩手标本及镜下照片

    Figure  2.  Manual samples and microscopic photographs of granodiorite porphyry

    图  3  代表性锆石阴极发光图像

    Figure  3.  Cathodoluminescence(CL) images of typical zircons

    图  4  尕尔勤花岗闪长斑岩稀土元素标准化图解

    Figure  4.  Standardization diagram of rare earth elements in granodiorite porphyry

    图  5  锆石稀土元素标准化图解

    Figure  5.  Standardization diagram of rare earth elements in zircon

    表  1  花岗闪长斑岩稀土元素测试分析表(×10-6)

    Table  1.   Test analysis table for rare earth elements of granodiorite porphyry

    序号 样号 岩性 La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
    1 DL025 花岗闪长斑岩 17.6 34.5 3.77 12.9 2.57 0.62 1.86 0.28 1.56 0.33 0.93 0.13 0.92 0.15
    2 DL027 花岗闪长斑岩 14.4 26.2 2.86 10.4 1.87 0.58 1.44 0.24 1.36 0.27 0.82 0.11 0.80 0.14
    3 DL031 花岗闪长斑岩 16.0 30.0 3.19 11.6 2.19 0.59 1.63 0.26 1.49 0.32 0.87 0.12 0.85 0.14
    4 DL033 花岗闪长斑岩 14.1 22.1 2.56 9.16 1.76 0.50 1.34 0.24 1.47 0.34 1.00 0.15 1.03 0.17
    5 DL037 花岗闪长斑岩 10.5 20.9 2.32 7.79 1.60 0.50 1.22 0.22 1.34 0.30 0.86 0.12 0.83 0.14
    下载: 导出CSV

    表  2  花岗闪长斑岩稀土元素相关参数计算

    Table  2.   Rare earth elements related parameter calculation of granodiorite porphyry

    序号 样号 LREE HREE L/H ΣREE La/Yb Sm/Nd Eu/Sm (La/Sm)N (Gd/Yb)N δCe δEu
    1 DL025 71.96 6.16 11.68 78.12 19.13 0.20 0.24 4.31 1.63 0.97 0.83
    2 DL027 56.31 5.18 10.87 61.49 18.00 0.18 0.31 4.84 1.45 0.93 1.04
    3 DL031 63.57 5.68 11.19 69.25 18.82 0.19 0.27 4.60 1.55 0.95 0.92
    4 DL033 50.18 5.74 8.74 55.92 13.69 0.19 0.28 5.04 1.05 0.82 0.96
    5 DL037 43.61 5.03 8.67 48.64 12.65 0.21 0.31 4.13 1.19 0.98 1.05
    下载: 导出CSV

    表  3  单颗粒锆石稀土元素LA-ICP-MS分析结果(×10-6)

    Table  3.   LA-ICP-MS Rare earth elements data of single grain zircon

    样品 La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu ΣREE L/H δCe δEu (La/Sm)N (Lu/Gd)N
    DL007-01 0.01 59.02 0.09 2.30 5.31 2.62 36.16 13.75 182.22 78.35 402.64 97.23 1045.11 246.87 2171.69 0.03 191.74 0.43 0.00 53.26
    DL007-02 0.03 31.64 0.06 0.91 2.67 1.43 18.09 7.30 102.66 47.24 252.58 65.34 739.84 190.28 1460.06 0.03 135.78 0.47 0.01 82.05
    DL007-03 0.00 33.44 0.09 1.47 2.68 1.64 21.26 8.02 108.37 50.00 271.72 70.18 784.29 202.28 1555.43 0.03 115.61 0.46 0.00 74.22
    DL007-04 0.14 34.74 0.14 2.04 4.12 1.93 24.68 8.94 117.70 51.36 268.49 64.81 738.05 182.95 1500.08 0.03 55.19 0.45 0.02 57.82
    DL007-05 0.09 30.17 0.05 0.77 2.12 0.84 10.44 4.20 54.58 23.55 126.01 31.69 360.45 90.83 735.78 0.05 112.33 0.45 0.03 67.84
    DL007-06 0.05 44.08 0.10 1.67 4.18 2.13 25.24 9.55 133.92 59.79 317.80 81.66 917.62 231.11 1828.90 0.03 112.90 0.49 0.01 71.43
    DL007-07 0.00 54.70 0.02 2.52 6.76 2.50 51.08 20.50 266.22 115.58 563.37 128.20 1301.24 284.79 2797.46 0.02 842.78 0.29 0.00 43.49
    DL007-08 1.15 34.40 0.32 2.01 3.02 1.52 18.16 6.86 90.41 40.55 212.63 54.12 616.05 154.21 1235.41 0.04 13.56 0.48 0.24 66.26
    DL007-09 0.21 45.81 0.17 2.05 5.32 2.12 25.53 8.67 117.42 49.28 248.21 59.33 657.05 157.01 1378.16 0.04 55.36 0.46 0.03 47.98
    DL007-10 0.00 44.55 0.03 1.65 4.87 1.50 33.87 14.51 204.75 93.72 486.29 121.06 1284.51 297.99 2589.30 0.02 392.23 0.26 0.00 68.64
    DL007-11 0.12 36.32 0.14 2.06 3.37 1.68 19.76 7.44 99.80 45.95 239.97 62.10 708.75 179.06 1406.49 0.03 58.88 0.49 0.02 70.70
    DL007-12 0.00 29.23 0.02 0.76 1.63 1.10 11.85 4.56 61.93 28.16 145.71 37.17 423.29 106.68 852.09 0.04 438.10 0.55 0.00 70.25
    DL007-13 0.02 58.84 0.17 1.87 6.29 2.34 41.59 15.86 207.85 89.80 455.47 111.93 1224.45 290.68 2507.15 0.03 101.28 0.33 0.00 54.52
    DL007-14 0.00 49.55 0.06 1.58 4.19 1.70 28.27 10.72 137.70 61.17 312.84 78.16 843.54 204.64 1734.13 0.03 232.58 0.35 0.00 56.46
    DL007-15 0.00 34.94 0.07 1.35 3.52 1.05 20.49 7.88 107.96 47.01 241.11 59.16 645.20 155.05 1324.77 0.03 153.61 0.29 0.00 59.03
    DL007-16 0.03 28.77 0.07 0.88 2.49 1.35 16.95 7.66 110.24 50.74 278.10 71.44 817.01 208.43 1594.16 0.02 107.11 0.47 0.01 95.94
    DL007-17 0.00 43.72 0.06 1.18 4.43 1.51 28.37 11.69 151.42 65.62 337.43 80.66 860.27 199.28 1785.63 0.03 232.02 0.31 0.00 54.80
    DL007-18 0.00 30.62 0.07 1.60 1.21 1.09 14.43 5.90 76.41 33.53 176.18 44.34 510.97 127.88 1024.23 0.03 127.90 0.48 0.00 69.12
    DL007-19 0.06 157.53 0.23 4.36 13.64 4.84 124.32 51.03 697.12 291.49 1391.49 312.44 3078.32 665.23 6792.10 0.03 190.58 0.24 0.00 41.75
    平均值 0.10 46.43 0.10 1.74 4.31 1.84 30.03 11.84 159.40 69.62 354.11 85.84 924.00 219.75 1909.11 0.03 193.13 0.41 0.02 63.45
    DL037-1 0.65 84.65 0.28 4.39 8.55 4.12 49.82 17.45 210.57 90.52 446.45 105.82 1119.54 270.40 2413.20 0.04 47.93 0.47 0.05 42.34
    DL037-2 0.00 37.92 0.06 1.42 3.81 1.65 27.82 10.69 145.48 60.11 310.51 75.20 801.92 194.14 1670.72 0.03 208.11 0.35 0.00 54.45
    DL037-3 0.04 47.72 0.16 1.91 5.48 1.91 38.09 16.12 224.18 94.36 486.35 116.40 1235.91 290.14 2558.77 0.02 83.57 0.30 0.00 59.42
    DL037-4 0.12 44.66 0.16 3.26 7.59 2.43 56.88 23.76 297.69 122.89 605.45 137.09 1385.14 305.45 2992.56 0.02 64.78 0.26 0.01 41.89
    DL037-5 0.03 39.13 0.04 1.42 4.09 2.01 26.92 9.70 130.52 56.82 304.80 74.86 846.32 210.87 1707.53 0.03 220.54 0.44 0.00 61.11
    DL037-8 0.34 33.20 0.46 4.17 3.89 2.56 17.17 7.03 88.12 39.45 208.20 54.36 623.82 160.12 1242.90 0.04 16.87 0.81 0.05 72.73
    DL037-9 0.00 135.15 0.27 4.35 14.12 7.35 73.10 26.19 324.32 135.07 674.09 160.15 1683.28 396.17 3633.63 0.05 148.64 0.56 0.00 42.28
    DL037-11 0.06 25.23 0.05 0.70 2.80 1.86 16.69 6.75 92.98 39.89 220.82 56.85 640.45 165.02 1270.14 0.02 97.83 0.64 0.01 77.15
    DL037-12 0.00 23.35 0.03 0.78 1.42 0.97 12.54 4.47 60.54 27.95 152.14 40.02 471.96 122.85 919.03 0.03 268.66 0.47 0.00 76.41
    DL037-13 0.01 73.97 0.14 3.01 8.59 3.70 42.32 15.00 204.39 88.31 454.27 111.08 1212.54 295.05 2512.38 0.04 158.39 0.48 0.00 54.40
    DL037-14 0.00 55.90 0.07 2.08 3.20 2.73 26.26 10.28 140.25 61.14 326.88 82.44 915.89 228.23 1855.36 0.04 225.36 0.63 0.00 67.80
    DL037-15 0.00 27.56 0.05 0.61 2.54 1.20 17.99 7.51 106.36 47.02 255.39 66.63 771.96 197.01 1501.82 0.02 159.22 0.40 0.00 85.42
    DL037-16 0.13 34.16 0.06 1.05 3.18 1.85 31.36 12.92 170.07 73.29 366.20 86.21 928.32 213.46 1922.24 0.02 94.19 0.37 0.03 53.10
    DL037-17 0.00 23.91 0.07 0.72 1.30 1.15 14.31 4.81 70.66 28.34 148.11 36.94 414.00 101.20 845.51 0.03 105.22 0.51 0.00 55.17
    DL037-18 0.00 17.09 0.06 0.76 1.73 0.87 12.85 4.65 57.67 27.06 146.53 39.59 433.91 111.44 854.21 0.02 88.54 0.41 0.00 67.64
    DL037-19 0.02 28.62 0.04 1.01 2.60 1.47 18.46 7.43 103.07 45.74 245.43 61.79 689.25 174.53 1379.45 0.03 188.32 0.47 0.00 73.75
    DL037-20 0.04 30.14 0.05 0.92 1.70 1.11 12.04 4.75 66.60 29.33 159.76 41.30 475.57 118.30 941.62 0.04 143.74 0.55 0.02 76.67
    平均值 0.08 44.85 0.12 1.92 4.50 2.29 29.10 11.15 146.67 62.78 324.20 79.22 861.75 209.08 1777.71 0.03 136.47 0.48 0.01 62.45
    下载: 导出CSV
  • [1] 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. http://www.cnki.com.cn/Article/CJFDTotal-YSXB200702002.htm

    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) http://www.cnki.com.cn/Article/CJFDTotal-YSXB200702002.htm
    [2] 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. http://www.doc88.com/p-3117968905923.html

    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) http://www.doc88.com/p-3117968905923.html
    [3] 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. https://www.researchgate.net/publication/297141458_Characteristics_of_rare_earth_elements_of_zircons_from_Mesozoic_volcanic_rocks_in_Luanping_region_Hebei
    [4] 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. https://www.wenkuxiazai.com/doc/9f9ff9758e9951e79b8927f5-3.html

    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) https://www.wenkuxiazai.com/doc/9f9ff9758e9951e79b8927f5-3.html
    [5] 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. http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20160515

    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) http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20160515
    [6] 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. http://d.old.wanfangdata.com.cn/Conference/8450798

    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) http://d.old.wanfangdata.com.cn/Conference/8450798
    [7] 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

    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
    [8] 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. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201702011

    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) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201702011
    [9] 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. http://d.old.wanfangdata.com.cn/Periodical/dzykt201202001

    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) http://d.old.wanfangdata.com.cn/Periodical/dzykt201202001
    [10] 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. http://d.old.wanfangdata.com.cn/Periodical/cdlgxyxb201401014

    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) http://d.old.wanfangdata.com.cn/Periodical/cdlgxyxb201401014
    [11] 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
    [12] 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.

    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)
    [13] 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
    [14] 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
    [15] 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
    [16] 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
    [17] 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. http://d.old.wanfangdata.com.cn/Periodical/zgxtxb201801015

    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) http://d.old.wanfangdata.com.cn/Periodical/zgxtxb201801015
    [18] 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. http://www.cqvip.com/QK/91256B/201204/43136177.html

    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) http://www.cqvip.com/QK/91256B/201204/43136177.html
    [19] 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
    [20] 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. http://industry.wanfangdata.com.cn/dl/Detail/Periodical?id=Periodical_dxqy201101023

    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) http://industry.wanfangdata.com.cn/dl/Detail/Periodical?id=Periodical_dxqy201101023
    [21] 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. http://www.cqvip.com/QK/91256B/201406/663466821.html

    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) http://www.cqvip.com/QK/91256B/201406/663466821.html
    [22] 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. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201703023.htm

    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) http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201703023.htm
    [23] 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. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-DZDQ200112001035.htm

    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) http://cpfd.cnki.com.cn/Article/CPFDTOTAL-DZDQ200112001035.htm
    [24] 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. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kcdz200906003

    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) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kcdz200906003
    [25] 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
    [26] 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
    [27] 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. http://d.old.wanfangdata.com.cn/Periodical/yskwxzz201406004

    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) http://d.old.wanfangdata.com.cn/Periodical/yskwxzz201406004
    [28] 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. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb201707009

    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) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb201707009
    [29] 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. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb201707010

    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) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb201707010
    [30] 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

    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) http://cdmd.cnki.com.cn/Article/CDMD-10616-1015312818.htm
    [31] 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. http://d.old.wanfangdata.com.cn/Periodical/yskwxzz201605008

    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) http://d.old.wanfangdata.com.cn/Periodical/yskwxzz201605008
    [32] 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. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200703021.htm

    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) http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200703021.htm
    [33] 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. http://www.ysxb.ac.cn/ysxb/ch/reader/create_pdf.aspx?file_no=20081202&journal_id=ysxb&year_id=2008

    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) http://www.ysxb.ac.cn/ysxb/ch/reader/create_pdf.aspx?file_no=20081202&journal_id=ysxb&year_id=2008
    [34] 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. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201001013.htm

    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) http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201001013.htm
    [35] 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. http://mall.cnki.net/magazine/Article/DXQY200402026.htm

    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) http://mall.cnki.net/magazine/Article/DXQY200402026.htm
    [36] 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. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201107008

    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) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201107008
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  • 收稿日期:  2017-07-09
  • 修回日期:  2018-05-20
  • 刊出日期:  2018-06-28

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