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云南省德钦县红坡牛场铜金矿区果腊复式岩体年龄、地球化学特征及其构造与找矿意义

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王小虎, 杨爱平, 李文辉, 杨淑胜, 范柱国, 谢志鹏, 卓伟峰. 云南省德钦县红坡牛场铜金矿区果腊复式岩体年龄、地球化学特征及其构造与找矿意义[J]. 地质通报, 2020, 39(2-3): 279-295.
引用本文: 王小虎, 杨爱平, 李文辉, 杨淑胜, 范柱国, 谢志鹏, 卓伟峰. 云南省德钦县红坡牛场铜金矿区果腊复式岩体年龄、地球化学特征及其构造与找矿意义[J]. 地质通报, 2020, 39(2-3): 279-295.
shu
WANG Xiaohu, YANG Aiping, LI Wenhui, YANG Shusheng, FAN Zhuguo, XIE Zhipeng, ZHUO Weifeng. Geochronology and geochemical characteristics of the Guola complex intrusion in the Hongponiuchang Cu-Au mining area of Deqin area, Yunnan Province, and its tectonic and prospecting significance[J]. Geological Bulletin of China, 2020, 39(2-3): 279-295.
Citation: WANG Xiaohu, YANG Aiping, LI Wenhui, YANG Shusheng, FAN Zhuguo, XIE Zhipeng, ZHUO Weifeng. Geochronology and geochemical characteristics of the Guola complex intrusion in the Hongponiuchang Cu-Au mining area of Deqin area, Yunnan Province, and its tectonic and prospecting significance[J]. Geological Bulletin of China, 2020, 39(2-3): 279-295.
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云南省德钦县红坡牛场铜金矿区果腊复式岩体年龄、地球化学特征及其构造与找矿意义

  • 1.

    云南省地质调查院, 云南 昆明 650216

  • 2.

    昆明理工大学国土资源工程学院, 云南 昆明 650093

  • 3.

    自然资源部三江成矿作用及资源勘查利用重点实验室, 云南 昆明 650061

  • 4.

    云南省国土资源规划设计研究院, 云南 昆明 650216

  • 5.

    德钦圣卓矿业有限公司, 云南 德钦 674500

  • 基金项目:
    云南省应用基础研究计划项目《滇西漕涧白垩纪花岗岩带的构造成因》（编号：2017FB075）和德钦圣卓矿业有限公司勘查项目《云南省德钦县红坡牛场铜金矿详查》（编号：HP2014-01）
详细信息
    作者简介: 王小虎(1986-), 男, 在读硕士生, 工程师, 从事矿产资源调查与评价。E-mail:339078312@qq.com
    通讯作者: 杨爱平(1963-), 男, 高级工程师, 从事矿产资源调查与评价、找矿预测。E-mail:15422576848@qq.com

  • 中图分类号: P618.41;P597+.3

Geochronology and geochemical characteristics of the Guola complex intrusion in the Hongponiuchang Cu-Au mining area of Deqin area, Yunnan Province, and its tectonic and prospecting significance

  • 1.

    Yunnan Institute of Geological Survey, Kunming 650216, Yunnan, China

  • 2.

    Faculty of Land Resources Engineering, Kunming University of Science and Technology, Kunming 650093, Yunnan, China

  • 3.

    Key Laboratory of Sanjiang Metallogeny and Resources Exploration and Utilization, Ministry of Land and Resources, Kunming 650061, Yunnan, China

  • 4.

    Yunnan Planning and Design Institute of Land Resources, Kunming 650216, Yunnan, China

  • 5.

    Deqin Shengzhuo Mining Co., Ltd., Deqin 674500, Yunnan, China

More Information

    摘要

  • 位于江达-维西火山弧铁-铜-铅-锌多金属成矿带的德钦县红坡牛场铜金矿床，是与果腊复式侵入体有关的矽卡岩型-热液型多金属矿床。LA-ICP-MS锆石U-Pb数据表明，复式岩体核部（石英二长岩）侵位年龄为226.4±2.0Ma，边部（石英闪长玢岩）为36.59±0.22 Ma，显示为印支期和喜马拉雅期2期岩浆活动的产物。核部石英二长岩具高SiO2（65.8%~68.5%）和低MgO（1.40%~2.17%）含量，属高钾钙碱性系列；高Sr，低Yb与Y含量证实其埃达克岩属性。地球化学特征及对比表明其很可能起源于加厚的陆壳底部，源区物质相当于榴辉岩的组成，而非俯冲洋壳熔融的产物。边部石英闪长玢岩具低SiO2（55.8%~56.6%），高MgO（6.45%~7.50%；Mg#=52.4~62）、Cr（228×10-6~353×10-6）和Ni（72.3×10-6~90.0×10-6），为典型的高镁闪长岩。地球化学特征显示其为下地壳物质在地幔深部发生熔融的产物。研究成果为金沙江古特提斯洋演化提供了新的年代学约束，在江达-维西火山弧带发现喜马拉雅期岩浆活动，对于重新认识该矿床成因及后续江达-维西带成矿规律总结和找矿方向具有重要的指导意义。

    The Hongponiuchang copper-gold deposit, located in the middle part of the Jiangda-Weixi volcanic arc Fe-Cu-Pb-Zn polymetallic metallogenic belt, is a skarn-hydrothermal polymetallic deposit related to the Guola complex intrusion.Zircon LA-ICP-MS U-Pb geochronology shows that the emplacement ages of the complex are 226.4±2.0 Ma and 36.59±0.22 Ma for the center (quartz monzonite) and the rim (quartz diorite porphyrite), respectively, suggesting that the complex represents the magmatic product of both Indosinian and Himalaya periods.The quartz monzonite as the center of complex has high SiO2 (65.8%~68.5%) and low MgO (1.40%~2.17%) content and represents high-K calc-alkali series; High Sr and low Yb and Y content indicates its adakitic characteristics.The geochemical characteristics and comparisons indicate that it was probably derived directly from the bottom of the thickened crust, with source material similar to the composition of the eclogite instead of the melting product of subduction oceanic crust.The quartz diorite porphyrite in the rims has low SiO2 (55.8%~56.6%) and high MgO (6.45%~7.50%), Cr (228×10-6~353×10-6), and Ni (72.3×10-6~90.0×10-6) values, indicating a typical high-magnesium diorite.Geochemical characteristics show that it is the product of melting of the lower crust at the depth of the mantle.This study has provided new geochronologic constraint for the evolution of the Jinshajiang Paleo-Tethys Ocean, and discovered the Himalayan magmatic activity in the Jiangda-Weixi arc belt, thus being of great significance to the genesis for the Hongponiuchang copper-gold deposit and the summary of the metallogenic regularity as well as the study of prospecting direction.

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  • 图 1  研究区地质简图

    Figure 1. 

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    图 图版Ⅰ   

    Figure 图版Ⅰ. 

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    图 2  红坡牛场铜金矿区果腊复式岩体岩浆锆石阴极发光(CL)图像及锆石206Pb/238U年龄

    Figure 2. 

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    图 3  果腊角闪石英二长岩和石英闪长玢岩LA-ICP-MS锆石U-Pb年龄谐和图

    Figure 3. 

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    图 4  滇西红坡牛场复式岩体全岩SiO2-K2O[29](a)和A/CNK-A/NK[30](b)图解

    Figure 4. 

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    图 5  滇西红坡牛场复式岩体稀土元素球粒陨石标准化分布图(a)和微量元素蛛网图(b)

    Figure 5. 

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    图 6  红坡牛场果腊复式岩体岩浆岩微量元素构造环境判别图解[52~53]

    Figure 6. 

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    表 1  云南省德钦县红坡牛场果腊复式岩体LA-ICP-MS锆石U-Th-Pb年龄数据

    Table 1.  LA-ICP-MS zircon U-Th-Pb data for Hongponiuchang Guola complex massif, Deqin County, Yunnan Province

    测点号 含量/10-6 Th/U 比值 年龄/Ma
    Th U Pb 207Pb/
    206Pb    		 1σ 207Pb/
    235U    		 1σ 206Pb/
    238U    		 1σ 207Pb/
    206Pb    		 1σ 207Pb/
    235U    		 1σ 206Pb/
    238U    		 1σ
    样品HPNC-1
    HPNC-1-2 92 121 57 0.76 0.0518 0.0005 0.2562 0.0027 0.03590 0.00022 276.0 20.4 231.6 2.2 227.4 1.4
    HPNC-1-3 109 155 73 0.70 0.0523 0.0005 0.2579 0.0032 0.03573 0.00027 301.9 24.1 233.0 2.6 226.3 1.7
    HPNC-1-4 80 109 62 0.74 0.0512 0.0008 0.2516 0.0041 0.03568 0.00023 255.6 35.2 227.9 3.3 226.0 1.5
    HPNC-1-6 101 129 55 0.78 0.0520 0.0006 0.2568 0.0029 0.03585 0.00025 287.1 30.6 232.1 2.3 227.1 1.6
    HPNC-1-7 416 338 229 1.23 0.0527 0.0005 0.2609 0.0028 0.03593 0.00027 322.3 25.0 235.4 2.3 227.6 1.7
    HPNC-1-8 112 169 62 0.66 0.0507 0.0004 0.2486 0.0025 0.03558 0.00021 227.8 23.1 225.5 2.0 225.3 1.3
    HPNC-1-9 141 167 62 0.84 0.0511 0.0005 0.2530 0.0029 0.03592 0.00024 255.6 50.0 229.0 2.3 227.5 1.5
    HPNC-1-10 106 113 44 0.93 0.0513 0.0012 0.2518 0.0078 0.03555 0.00047 253.8 47.2 228.0 6.3 225.2 2.9
    HPNC-1-11 226 176 107 1.29 0.0512 0.0005 0.2522 0.0028 0.03571 0.00022 250.1 22.2 228.3 2.2 226.2 1.4
    HPNC-1-12 169 211 93 0.80 0.0509 0.0006 0.2507 0.0032 0.03572 0.00023 235.3 25.9 227.1 2.6 226.3 1.4
    HPNC-1-13 182 247 93 0.74 0.0508 0.0003 0.2492 0.0021 0.03557 0.00021 231.6 19.4 225.9 1.7 225.3 1.3
    HPNC-1-14 118 184 59 0.64 0.0519 0.0005 0.2572 0.0032 0.03593 0.00030 283.4 22.2 232.4 2.6 227.5 1.9
    HPNC-1-15 192 183 92 1.05 0.0509 0.0004 0.2507 0.0021 0.03576 0.00020 235.3 16.7 227.2 1.7 226.5 1.3
    HPNC-1-16 79 92 49 0.85 0.0540 0.0027 0.2640 0.0106 0.03558 0.00054 372.3 113.0 237.9 8.5 225.4 3.3
    HPNC-1-18 172 205 137 0.84 0.0510 0.0011 0.2504 0.0063 0.03560 0.00036 239.0 54.6 226.9 5.1 225.5 2.2
    HPNC-1-19 395 299 171 1.32 0.0508 0.0006 0.2492 0.0031 0.03560 0.00026 231.6 23.1 225.9 2.5 225.5 1.6
    样品HPNC-2
    HPNC-2-2 1620 2630 28 0.62 0.0457 0.0028 0.0394 0.0023 0.00584 0.00012 -10.0 120.0 39.2 2.2 37.6 0.8
    HPNC-2-3 493 818 9 0.60 0.0446 0.0032 0.0344 0.0025 0.00559 0.00009 -20.0 130.0 34.2 2.4 36.0 0.6
    HPNC-2-4 734 1460 13 0.50 0.0480 0.0023 0.0377 0.0017 0.00564 0.00007 109.0 93.0 37.6 1.7 36.2 0.5
    HPNC-2-5 1259 1667 21 0.76 0.0482 0.0021 0.0380 0.0017 0.00569 0.00007 118.0 87.0 37.8 1.6 36.5 0.5
    HPNC-2-7 1042 1553 18 0.67 0.0474 0.0024 0.0375 0.0019 0.00563 0.00008 66.0 97.0 37.2 1.8 36.2 0.5
    HPNC-2-10 764 1427 13 0.54 0.0471 0.0024 0.0373 0.0020 0.00583 0.00009 60.0 100.0 37.3 2.0 37.5 0.6
    HPNC-2-11 374 828 6 0.45 0.0432 0.0030 0.0347 0.0024 0.00566 0.00009 -30.0 120.0 34.7 2.4 36.4 0.6
    HPNC-2-12 679 1374 12 0.49 0.0462 0.0025 0.0374 0.0020 0.00582 0.00008 40.0 100.0 37.3 1.9 37.4 0.5
    HPNC-2-13 742 1010 13 0.73 0.0441 0.0031 0.0350 0.0024 0.00579 0.00010 -80.0 120.0 34.8 2.3 37.2 0.7
    HPNC-2-14 737 1120 13 0.66 0.0438 0.0029 0.0352 0.0024 0.00570 0.00010 -40.0 120.0 34.9 2.3 36.6 0.6
    HPNC-2-15 4258 4134 74 1.03 0.0455 0.0016 0.0353 0.0012 0.00563 0.00007 -20.0 68.0 35.2 1.1 36.2 0.4
    HPNC-2-17 761 1103 13 0.69 0.0461 0.0030 0.0366 0.0022 0.00567 0.00009 20.0 120.0 36.4 2.2 36.4 0.6
    HPNC-2-18 1783 2487 31 0.72 0.0483 0.0018 0.0374 0.0015 0.00573 0.00008 114.0 77.0 37.5 1.4 36.8 0.5
    HPNC-2-19 2343 4430 40 0.53 0.0464 0.0016 0.0376 0.0012 0.00571 0.00007 41.0 68.0 37.5 1.2 36.7 0.5
    HPNC-2-20 546 1294 9 0.42 0.0478 0.0029 0.0362 0.0021 0.00562 0.00009 70.0 120.0 36.0 2.1 36.1 0.5
    HPNC-2-21 1154 1463 19 0.79 0.0489 0.0025 0.0378 0.0018 0.00561 0.00008 151.0 97.0 37.6 1.8 36.1 0.5
    HPNC-2-22 5300 4670 88 1.13 0.0456 0.0019 0.0379 0.0017 0.00575 0.00011 6.0 84.0 37.8 1.7 36.9 0.7
    HPNC-2-23 1196 1510 20 0.79 0.0440 0.0023 0.0347 0.0018 0.00567 0.00008 -70.0 98.0 34.6 1.8 36.4 0.5
    HPNC-2-24 885 1178 14 0.75 0.0435 0.0028 0.0351 0.0022 0.00567 0.00009 -70.0 120.0 35.2 2.1 36.4 0.6
    HPNC-2-25 1607 2194 26 0.73 0.0443 0.0020 0.0345 0.0015 0.00568 0.00007 -89.0 86.0 34.5 1.5 36.5 0.5
    HPNC-2-26 1247 1739 21 0.72 0.0458 0.0022 0.0368 0.0018 0.00577 0.00008 -5.0 92.0 36.6 1.7 37.1 0.5
    HPNC-2-27 398 863 7 0.46 0.0453 0.0031 0.0357 0.0024 0.00558 0.00010 60.0 120.0 35.4 2.4 35.9 0.6
    HPNC-2-30 3710 3846 67 0.96 0.0474 0.0015 0.0379 0.0012 0.00578 0.00007 70.0 66.0 37.7 1.2 37.2 0.5
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    表 2  红坡牛场复式岩体全岩主量、微量和稀土元素含量

    Table 2.  The major, trace and rare earth elements data for the Hongponiuchang igneous complex

    岩性 角闪石英二长岩 石英闪长玢岩
    样号 HPGXW1 HPGXW4 HPGXW5 HPGXW2 HPGXW3
    SiO2 67.95 65.8 68.49 55.77 56.58
    TiO2 0.31 0.41 0.32 0.35 0.67
    Al2O3 13.98 14.09 13.93 12.43 12.2
    Fe2O3 4.62 2.73 2.62 7.7 2.76
    FeO 1.8 1.81 1.63 5.2 4.56
    MgO 1.4 2.17 1.4 7.5 6.45
    MnO 0.04 0.05 0.03 0.12 0.12
    CaO 1.93 2.16 1.19 7.39 7.35
    P2O5 0.16 0.25 0.17 0.55 0.56
    Na2O 3.65 3.84 3.88 2.44 2.68
    K2O 5.06 5.48 4.51 5.06 5.18
    烧失量 0.65 0.87 0.54 0.20 0.63
    总计 101.55 99.66 98.71 104.71 99.74
    V 49.8 87.5 76.2 171 108
    Cr 42.4 81.4 71.9 353 228
    Co 6.9 9.9 6.25 25.3 29.2
    Ni 19 24.8 18.6 90 72.3
    Cu 27 19.2 49.1 62.6 59.4
    Zn 55.1 33 24 86 68
    Rb 291 258 232 258 229
    Sr 604 633 450 933 940
    Y 14.8 16.7 14 20.8 20.6
    Zr 252 265 234 150 180
    Nb 16.7 18 14.1 10.4 10.9
    Ba 772 910 670 1370 1374
    La 34.3 38 34.3 27.2 30
    Ce 59.9 68.9 63.3 52.5 60.7
    Pr 6.94 7.97 7.19 7.11 7.9
    Nd 25 29.8 25.9 29.9 33.4
    Sm 4.28 5.31 4.51 6.16 6.65
    Eu 1.08 1.2 0.98 1.68 1.66
    Gd 4.02 4.86 4.18 5.54 5.87
    Tb 0.54 0.65 0.56 0.8 0.84
    Dy 2.77 3.4 2.84 4.25 4.47
    Ho 0.52 0.63 0.53 0.8 0.81
    Er 1.57 1.82 1.59 2.22 2.28
    Tm 0.23 0.26 0.23 0.3 0.31
    Yb 1.47 1.7 1.51 1.92 2.02
    Lu 0.23 0.25 0.22 0.3 0.3
    Hf 7.23 3.18 2.59 4.88 5.38
    Ta 1.83 0.92 0.82 1.58 0.6
    Pb 84.3 32.8 26.8 61.3 42
    Th 40.5 30.8 32.3 14.7 13
    U 15.3 11.5 7.34 6.45 6.51
    A/CNK 0.94 0.88 1.04 0.55 0.53
    A/NK 1.22 1.15 1.24 1.31 1.22
    Na2O/K2O 0.72 0.70 0.86 0.48 0.52
    Na2O+K2O 8.71 9.32 8.39 7.50 7.86
    ∑REE 142.85 164.75 147.84 140.68 157.21
    LaN/YbN 15.85 15.18 15.43 9.62 10.09
    DyN/YbN 1.23 1.31 1.23 1.45 1.45
    Eu/Eu* 0.79 0.72 0.69 0.88 0.81
    下载: 导出CSV
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收稿日期:  2018-11-23
修回日期:  2019-01-07
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