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    西藏玉龙铜矿带包买矿床含矿斑岩锆石U-Pb年代学

    林彬 王立强 唐菊兴 宋扬 周新 刘治博 高一鸣 唐晓倩 徐瑞阁 陈早军

    林彬, 王立强, 唐菊兴, 宋扬, 周新, 刘治博, 高一鸣, 唐晓倩, 徐瑞阁, 陈早军, 2017. 西藏玉龙铜矿带包买矿床含矿斑岩锆石U-Pb年代学. 地球科学, 42(9): 1454-1471. doi: 10.3799/dqkx.2017.517
    引用本文: 林彬, 王立强, 唐菊兴, 宋扬, 周新, 刘治博, 高一鸣, 唐晓倩, 徐瑞阁, 陈早军, 2017. 西藏玉龙铜矿带包买矿床含矿斑岩锆石U-Pb年代学. 地球科学, 42(9): 1454-1471. doi: 10.3799/dqkx.2017.517
    Lin Bin, Wang Liqiang, Tang Juxing, Song Yang, Zhou Xin, Liu Zhibo, Gao Yiming, Tang Xiaoqian, Xu Ruige, Chen Zaojun, 2017. Zircon U-Pb Geochronology of Ore-Bearing Porphyries in Baomai Deposit, Yulong Copper Belt, Tibet. Earth Science, 42(9): 1454-1471. doi: 10.3799/dqkx.2017.517
    Citation: Lin Bin, Wang Liqiang, Tang Juxing, Song Yang, Zhou Xin, Liu Zhibo, Gao Yiming, Tang Xiaoqian, Xu Ruige, Chen Zaojun, 2017. Zircon U-Pb Geochronology of Ore-Bearing Porphyries in Baomai Deposit, Yulong Copper Belt, Tibet. Earth Science, 42(9): 1454-1471. doi: 10.3799/dqkx.2017.517

    西藏玉龙铜矿带包买矿床含矿斑岩锆石U-Pb年代学

    doi: 10.3799/dqkx.2017.517
    基金项目: 

    国家自然科学基金 41402178

    中国地质调查局公益性行业科研专项 201511017

    中国地质调查局公益性行业科研专项 201511022-02

    中国地质科学院基本科研业务费 YYWF201608

    国家自然科学基金 41403040

    详细信息
      作者简介:

      林彬(1987-), 男, 博士研究生, 主要从事矿物学、岩石学、矿床学研究

    • 中图分类号: P597

    Zircon U-Pb Geochronology of Ore-Bearing Porphyries in Baomai Deposit, Yulong Copper Belt, Tibet

    • 摘要: 包买斑岩型铜钼矿床是西藏玉龙铜矿带北段重要组成部分,具有典型的斑岩型矿化、蚀变特征.最新勘查进展揭示其铜、钼资源量均已达中型矿床规模,但理论研究工作仍十分薄弱.以矿区基本地质特征为基础,运用LA-ICP-MS锆石U-Pb年代学方法,精确获得包买矿区与成矿有关的黑云母花岗岩和黑云母二长花岗岩侵位时代分别为:41.3±0.2 Ma和40.8±0.2 Ma,与玉龙、扎那尕等矿床一致,是始新世印度大陆与欧亚大陆碰撞造山过程的产物.综合区域已有年代学证据,玉龙铜矿带与成矿有关的斑岩体主要集中侵位于37~42 Ma,可能不存在明显的早(51 Ma)、中(41 Ma)、晚(33 Ma)三期,且从北西向南东,成岩成矿时代也没有明显降低变新的趋势.

       

    • 图  1  西藏玉龙斑岩铜矿带区域构造位置

      Hou et al.(2003c)唐菊兴等(2006)以及陈喜连等(2016)

      Fig.  1.  Regional tectonic location of the Yulong porphyry copper belt

      图  2  西藏包买斑岩铜钼矿矿区地质图

      据李伟(2014)

      Fig.  2.  Geological sketch of Baomai porphyry copper-molybdenite deposit in Tibet

      图  3  包买斑岩铜钼矿床02号剖面

      a.ZK0208-206.5 m辉钼矿化角砾岩;b.ZK0208-220.0 m闪长岩脉;c.ZK0208-231.0 m裂隙面上辉钼矿化;d.ZK0208-266.3 m含矿斑岩中石英-硫化物脉.Mol.辉钼矿;Cp.黄铜矿;Q-sulfide vein.石英-硫化物脉

      Fig.  3.  No.2 section of Baomai porphyry Cu (Mo) deposit, Tibet

      图  4  包买斑岩铜钼矿床主要矿化特征及岩石组成

      a.ZK0208-200.3 m泥化蚀变黑云母花岗岩中的硫化物脉;b.ZK0208-200.3 m硫化物脉中Cp、Eg、Py(反射光);c.ZK0208-271.0 m黑云母花岗岩,裂隙面上可见细粒辉钼矿;d.ZK0507-792.7 m黑云母二长花岗岩石英-辉钼矿-黄铜矿脉;e.ZK0607-207.1 m黄铜矿化片麻岩;f.ZK0607-207.1 m片麻岩(正交偏光).Q.石英;Mol.辉钼矿;Cp.黄铜矿;Eg.硫砷铜矿;Py.黄铁矿;Bio.黑云母;Pl.斜长石;Kfs.钾长石

      Fig.  4.  Mineralized characteristics and petrology of Baomai porphyry Cu (Mo) deposit, Tibet

      图  5  包买矿床含矿斑岩部分锆石CL图及U-Pb测点

      a.样品1,黑云母花岗斑岩(ZK0208-266.0 m);b.样品2,黑云母二长花岗岩(ZK0507-789.2 m)

      Fig.  5.  CL diagram of part of zircons and analysis point in ore-bearing porphyry of Baomai deposit, Tibet

      图  6  包买矿床含矿斑岩U-Pb谐和年龄

      Fig.  6.  U-Pb zircon concordia plots for ore-bearing porphyry of Baomai deposit, Tibet

      图  7  西藏玉龙铜矿带斑岩体同位素年龄值直方图

      数据来源见表 3

      Fig.  7.  Histogram of isotopic ages of porphyry bodies in the Yulong porphyry copper belt, Tibet

      图  8  西藏玉龙铜矿带成岩成矿时代分布

      数据来源见表 3

      Fig.  8.  Distribution diagram of isotopic ages in the Yulong porphyry copper belt, Tibet

      表  1  包买铜钼矿床含矿斑岩锆石LA-ICP-MS U-Pb分析结果

      Table  1.   Zircon LA-ICP-MS U-Pb ages of the Baomai ore-bearing porphyry

      样品编号Th(10-6)U(10-6)Th/U207Pb/206Pb1σ207Pb/235U1σ206Pb/238U1σ206Pb/238U(Ma)1σ
      黑云母花岗岩
      ZK0208-266.0 m-16299030.70.051 60.003 20.044 60.002 90.006 30.000 140.70.8
      ZK0208-266.0 m-24979580.50.051 50.003 70.044 40.003 20.006 20.000 140.10.7
      ZK0208-266.0 m-41 5311 6260.90.052 30.004 40.045 50.003 60.006 40.000 141.00.8
      ZK0208-266.0 m-56751 2940.50.052 10.002 60.045 40.002 20.006 30.000 140.80.5
      ZK0208-266.0 m-66861 1610.60.052 40.002 20.045 80.001 80.006 40.000 141.20.5
      ZK0208-266.0 m-71 7232 4970.70.048 10.002 30.041 40.001 90.006 30.000 140.20.5
      ZK0208-266.0 m-97891 3600.60.051 00.002 00.044 20.001 60.006 40.000 141.30.5
      ZK0208-266.0 m-106081 2050.50.050 90.002 90.044 00.002 50.006 40.000 140.90.6
      ZK0208-266.0 m-113541 1240.30.050 60.002 50.044 20.002 20.006 50.000 141.70.6
      ZK0208-266.0 m-125411 0830.50.051 80.002 30.045 20.002 10.006 40.000 141.20.6
      ZK0208-266.0 m-131 0682 0500.50.048 20.001 90.042 90.001 80.006 50.000 141.60.5
      ZK0208-266.0 m-144831 1940.40.050 10.002 60.044 30.002 30.006 60.000 142.10.6
      ZK0208-266.0 m-156111 3430.50.047 70.002 70.042 80.002 30.006 50.000 141.90.5
      ZK0208-266.0 m-167451 4240.50.049 90.002 20.044 30.002 00.006 50.000 141.70.5
      ZK0208-266.0 m-197291 0140.70.048 10.007 20.042 40.006 70.006 50.000 241.71.4
      ZK0208-266.0 m-207441 1880.60.052 20.002 60.045 30.002 10.006 50.000 141.70.6
      ZK0208-266.0 m-211 6421 9900.80.050 70.002 10.044 20.001 90.006 30.000 140.70.5
      ZK0208-266.0 m-223167130.40.050 50.008 10.040 60.004 80.006 20.000 340.02.0
      ZK0208-266.0 m-234696880.70.052 70.019 90.044 30.012 90.006 40.000 541.32.9
      ZK0208-266.0 m-247071 6100.40.051 20.002 80.043 70.002 30.006 30.000 140.30.5
      ZK0208-266.0 m-256189000.70.052 70.002 70.046 00.002 30.006 50.000 141.50.6
      ZK0208-266.0 m-267391 5830.50.051 00.002 20.044 80.002 00.006 40.000 141.10.5
      ZK0208-266.0 m-271 3812 2040.60.048 90.002 00.043 40.001 80.006 50.000 141.90.5
      ZK0208-266.0 m-281 6971 3171.30.050 00.003 00.044 10.002 60.006 50.000 141.70.6
      ZK0208-266.0 m-297831 5990.50.046 20.002 10.041 00.001 90.006 50.000 141.80.6
      ZK0208-266.0 m-301 1821 2460.90.052 20.002 70.045 50.002 40.006 40.000 141.10.7
      黑云母二长花岗岩
      ZK0507-789.2 m-15921 0140.60.043 40.002 80.037 40.002 50.006 20.000 140.20.6
      ZK0507-789.2 m-26611 0760.60.052 70.002 00.046 30.002 00.006 30.000 140.60.5
      ZK0507-789.2 m-35411 5140.40.050 50.001 70.043 30.001 50.006 30.000 140.40.5
      ZK0507-789.2 m-53769050.40.051 40.003 00.046 20.002 90.006 50.000 141.60.8
      ZK0507-789.2 m-61 1001 6890.70.052 60.004 60.044 30.003 40.006 20.000 140.10.8
      ZK0507-789.2 m-78441 6650.50.050 60.002 70.043 50.002 30.006 20.000 140.10.6
      ZK0507-789.2 m-86231 3460.50.052 80.004 60.045 40.003 80.006 40.000 141.20.9
      ZK0507-789.2 m-97261 3650.50.050 90.002 70.043 60.002 20.006 30.000 140.30.7
      ZK0507-789.2 m-109511 5550.60.048 30.003 50.041 30.002 90.006 20.000 140.10.8
      ZK0507-789.2 m-118071 2480.70.051 80.002 70.044 90.002 40.006 30.000 140.30.5
      ZK0507-789.2 m-128481 5050.60.050 30.002 40.043 10.002 00.00630.000 140.30.5
      ZK0507-789.2 m-136481 4370.50.048 50.002 10.042 40.001 80.006 40.000 140.90.5
      ZK0507-789.2 m-147461 1250.70.051 30.002 10.044 60.001 80.006 40.000 141.00.5
      ZK0507-789.2 m-151 0021 6480.60.051 20.001 90.045 30.001 70.006 40.000 141.20.5
      ZK0507-789.2 m-167121 4810.50.050 20.002 00.043 80.001 90.006 40.000 141.20.6
      ZK0507-789.2 m-176291 5860.40.050 70.002 20.043 20.001 80.006 20.000 140.00.5
      ZK0507-789.2 m-188721 4440.60.049 10.002 10.042 50.001 80.00630.000 140.60.5
      ZK0507-789.2 m-191 0351 0591.00.050 30.004 00.042 80.003 50.006 20.000 139.60.8
      ZK0507-789.2 m-205441 2420.40.049 80.002 30.043 50.002 10.006 30.000 140.70.5
      ZK0507-789.2 m-212826440.40.054 30.004 40.044 80.003 20.006 20.000 240.21.0
      ZK0507-789.2 m-225171 1440.50.047 50.002 00.041 40.001 70.006 40.000 141.20.5
      ZK0507-789.2 m-237321 5660.50.050 50.002 10.044 60.001 90.006 50.000 141.60.5
      ZK0507-789.2 m-241 0111 1820.90.049 90.002 40.044 40.002 10.006 50.000 141.80.6
      ZK0507-789.2 m-259751 5200.70.044 70.002 20.039 40.002 00.006 50.000 141.50.6
      ZK0507-789.2 m-261 0511 3990.80.051 70.002 30.045 20.001 90.006 50.000 141.60.5
      ZK0507-789.2 m-274791 0150.50.05210.002 60.045 80.002 10.006 50.000 141.70.6
      ZK0507-789.2 m-289201 4070.70.049 60.002 00.043 50.001 80.006 40.000 141.10.5
      ZK0507-789.2 m-299931 2920.80.051 50.002 30.043 80.001 90.006 30.000 140.30.5
      ZK0507-789.2 m-306061 0490.60.051 10.004 80.045 60.004 10.006 50.000 241.91.2
        注:测试单位为中国地质科学院矿产资源研究所,测试者为王倩,测试手段为激光剥蚀-等离子体质谱仪(LA-ICP-MS).
      下载: 导出CSV

      表  2  玉龙铜矿带各矿床地质特征对比

      Table  2.   Comparison of the characteristics of deposits in Yulong copper belt

      矿床纳日贡玛包买玉龙扎那尕多霞松多马拉松多色礼马牧普总郭
      控矿
      构造
      受NW-SE向深大断裂控制,位于杂多复式背斜北翼,发育NE、EW、NS向小断裂受控于NW-SE向走滑断裂系统及夏日多背斜,矿区发育多组小断裂受控于金沙江-红河断裂,位于恒星错-甘龙拉短轴背斜南端转转端受控于NW-SE向走滑断裂系统受控于NW-SE向走滑断裂, 莽总背斜中段受控于NW-SE向走滑断裂系统受控于近南北向红河-哀牢山断裂,产于色礼背斜核部受控于近南北向红河-哀牢山断裂,产于吉措背斜南段西翼受控于近南北向红河-哀牢山断裂,产于色礼背斜核部
      赋矿
      地层
      下二叠统开心岭群中基性火山熔岩早元古生界宁多岩群片麻岩和中三叠统夏日多组灰岩、页岩上三叠统灰岩、凝灰质泥岩,粉砂岩,砂岩下二叠统火山岩及上三叠统甲丕拉组砂泥岩上三叠统砂岩、粉砂岩、泥岩和页岩上三叠统甲丕拉组泥岩、粉砂岩及下三叠统流纹岩和凝灰岩晚三叠统砂页岩晚三叠统砂页岩和二叠-白垩系砂砾岩中晚三叠统巴贡组紫红色砂砾岩及页岩夹凝灰岩、灰岩
      岩体特征含矿斑岩主要为黑云母花岗斑岩黑云母花岗斑岩,黑云母二长花岗岩黑云母二长花岗斑岩,其次为花岗闪长斑岩、碱长花岗岩二长花岗斑岩,正长花岗斑岩二长花岗斑岩和碱长花岗斑岩,正常花岗斑岩碱长花岗斑岩二长花岗斑岩正长斑岩石英二长斑岩
      蚀变特征发育石英-绢云母化、青磐岩化、钾硅酸盐化、泥化发育绢云母化、钾硅酸盐化、泥化、矽卡岩化发育钾硅酸盐化、石英-绢云母化,泥化,青磐岩化;矽卡岩化发育钾硅化,黄铁绢英岩化,泥化,青磐岩化钾硅酸盐化、石英-绢云母化,青磐岩化钾长石化、硅化、绢云母化和泥化绿帘石化、绿泥石化角岩化、绿泥石化、绿帘石化-
      矿体形态条带状、透镜状脉状、透镜状产出矽卡岩型层状矿体,斑岩型透镜状矿体柱状,透镜状不规则状,透镜状透镜状、不规则状不规则状不规则状-
      矿石类型细脉-细脉状产出浸染状,细脉状,脉状细脉浸染状、网脉状、块状细脉浸染状细脉浸染状,网脉状细脉浸染状浸染状浸染状-
      矿物组合黄铜矿、辉钼矿、辉铜矿、蓝铜矿、黄铁矿黄铜矿、辉钼矿、黄铁矿、硫砷铜矿黄铜矿、辉钼矿、黄铁矿、斑铜矿、辉铜矿、赤铜矿黄铜矿、辉钼矿、黄铁矿、磁铁矿、辉铜矿等,偶见方铅矿、闪锌矿等黄铜矿、黄铁矿、少量辉钼矿、斑铜矿、磁铁矿黄铜矿、黄铁矿、辉钼矿、方铅矿、闪锌矿等黄铜矿、辉钼矿黄铜矿、黄铁矿黄铜矿
      成矿元
      素组合
      Cu、MoCu、Mo、Fe、AsCu、Mo、Fe、W、Au、Ag、Pb、Zn、Ni、CoCu、Mo、Au、FeCu、Mo、Au、AgCu、Mo、Au、Ag、PGECu、MoCu、Au、AgCu
      矿床规模中型;Cu金属量25万t@0.33%,Mo金属量68万t中型:Cu金属量21万t@0.22%;Mo金属量6万t@0.06%超大型:Cu资源量6.22 Mt@0.99%,Mo@0.028%,0.35 g/t中型:Cu金属量30万t@0.36%;Mo@0.03%,Au0.03 g/t大型:Cu金属量50万t@0.38%,Mo@0.04%,Au@0.05 g/t大型:Cu金属量100万t@0.44%;Mo 0.014%矿化点矿化点矿化点
      参考文献杨志明等, 2008王召林等, 2008本文吴伟中等, 2013何国朝等, 2014吴伟中等, 2013梁华英等, 2009陈喜连等, 2016陈喜连等, 2016陈喜连等, 2016
        注:@表示平均品位;“-”表示暂无相关资料.
      下载: 导出CSV

      表  3  西藏玉龙铜矿带年代学数据

      Table  3.   Geochronology of Yulong porphyry copper belt, Tibet

      矿区岩石类型测试对象矿化特征测试方法年龄(Ma)均值(Ma)数据来源处理
      纳日贡玛辉钼矿辉钼矿矿化Re-Os40.840.9郝金华等,2012
      石英-辉钼矿脉辉钼矿矿化Re-Os40.9王召林等,2008
      黑云母花岗斑岩锆石含矿LA U-Pb43.442.3郝金华等,2012
      黑云母花岗斑岩锆石含矿LA U-Pb42.9郝金华等,2012
      黑云母花岗斑岩锆石含矿LA U-Pb41.5宋忠宝等,2011
      花岗闪长斑岩锆石含矿LA U-Pb41.4宋忠宝等,2011
      斜长花岗斑岩锆石含矿LA U-Pb41.0宋忠宝等,2011
      黑云母花岗斑岩锆石含矿SHRIMP43.3杨志明等,2008
      日胆果二长花岗斑岩长石含矿K-Ar41.541.5Hou et al., 2003c参考
      二长花岗斑岩钾长石含矿K-Ar41.5Hou et al., 2003c参考
      夏日多二长花岗斑岩钾长石无矿K-Ar46.0马鸿文,1990删除
      包买黑云母花岗岩锆石含矿LA U-Pb41.341.1本文
      黑云母二长花岗岩锆石含矿LA U-Pb40.8本文
      恒星错花岗闪长岩钾长石含矿K-Ar40.7刘荣谟和赵定华, 1981参考
      二长花岗斑岩钾长石含矿K-Ar41.541.3唐仁鲤和罗怀松, 1995参考
      二长花岗斑岩钾长石含矿K-Ar41.0唐仁鲤和罗怀松, 1995参考
      二长花岗斑岩全岩含矿K-Ar42.7刘荣谟和赵定华, 1981删除
      玉龙二长花岗斑岩黑云母含矿K-Ar40.7马鸿文,1989b删除
      二长花岗斑岩黑云母含矿K-Ar48.2马鸿文,1989b删除
      二长花岗斑岩黑云母含矿K-Ar41.5刘荣谟和赵定华, 1981删除
      二长花岗斑岩钾长石含矿K-Ar40.0刘荣谟和赵定华, 1981删除
      二长花岗斑岩钾长石含矿K-Ar37.9刘荣谟和赵定华, 1981删除
      二长花岗斑岩钾长石含矿K-Ar38.2刘荣谟和赵定华, 1981删除
      二长花岗斑岩钾长石含矿K-Ar55.0马鸿文,1989b删除
      二长花岗斑岩钾长石含矿K-Ar55.0马鸿文,1989b删除
      二长花岗斑岩黑云母含矿Rb-Sr41.0马鸿文,1989b删除
      二长花岗斑岩黑云母含矿Rb-Sr41.0马鸿文,1989b删除
      二长花岗斑岩钾长石含矿K-Ar38.0张玉泉等,1987删除
      二长花岗斑岩钾长石含矿K-Ar41.0张玉泉等,1987删除
      二长花岗斑岩黑云母含矿Ar-Ar52.8马鸿文,1989b删除
      二长花岗斑岩黑云母含矿Rb-Sr52.0马鸿文,1989b删除
      石英-辉钼矿脉辉钼矿含矿Re-Os40.140.9曾普胜等,2006
      石英-辉钼矿脉辉钼矿含矿Re-Os41.6唐菊兴等,2009
      石英二长花岗斑岩锆石成矿前LA U-Pb41.342.1梁华英等,2008
      含矿斑岩锆石含矿LA U-Pb41.2Liang et al., 2006
      二长花岗岩锆石含矿SHRIMP40.9曾普胜等,2006
      石英二长斑岩锆石成矿前SHRIMP43.6郭利果等,2006
      黑云母二长花岗斑岩锆石含矿SHRIMP41.0郭利果等,2006
      黑云母二长花岗斑岩锆石含矿SHRIMP43.8王成辉等,2009
      黑云母二长花岗斑岩锆石含矿SHRIMP43.0王成辉等,2009
      正长花岗斑岩黑云母含矿Ar-Ar41.7梁华英等,2008
      玉龙北甘龙拉石英斜长斑岩锆石含矿SHRIMP43.9王成辉等,2009
      玉龙南纳加石英二长花岗斑岩锆石无矿SHRIMP41.4王成辉等,2009
      扎那尕二长花岗斑岩黑云母含矿K-Ar40.0张玉泉等,1987删除
      二长花岗斑岩钾长石含矿K-Ar33.9刘荣谟和赵定华, 1981删除
      二长花岗斑岩钾长石含矿K-Ar34.0张玉泉等,1987删除
      含矿斑岩锆石含矿LA U-Pb38.538.5Liang et al., 2006
      莽总二长花岗斑岩钾长石含矿K-Ar33.9刘荣谟和赵定华, 1981删除
      二长花岗斑岩锆石含矿LA U-Pb37.637.6Liang et al., 2006
      二长花岗斑岩钾长石含矿K-Ar42.7马鸿文等,1989b删除
      多霞松多含矿斑岩锆石含矿LA U-Pb37.537.5Liang et al., 2006
      花岗斑岩锆石含矿U-Pb41.0马鸿文等,1990删除
      二长花岗斑岩全岩含矿Rb-Sr52.0马鸿文等,1990删除
      马拉松多花岗斑岩锆石含矿U-Pb41.0马鸿文等,1990删除
      正长花岗斑岩钾长石含矿K-Ar35.8唐仁鲤和罗怀松, 1995删除
      二长花岗斑岩锆石含矿U-Pb40.9马鸿文等,1990删除
      二长花岗斑岩全岩含矿K-Ar50.9唐仁鲤等., 1995删除
      石英二长斑岩锆石成矿前LA U-Pb36.936.9梁华英等,2009
      碱长花岗斑岩锆石含矿LA U-Pb36.9梁华英等,2009
      碱长花岗斑岩黑云母含矿K-Ar36.9梁华英等,2009
      石英-辉钼矿脉辉钼矿含矿Re-Os35.935.8唐仁鲤和罗怀松, 1995
      石英-辉钼矿脉辉钼矿含矿Re-Os35.4唐仁鲤和罗怀松, 1995
      石英-辉钼矿脉辉钼矿含矿Re-Os36.2唐仁鲤和罗怀松, 1995
      石英-辉钼矿脉辉钼矿含矿Re-Os35.8杜安道等,1994
      拉日玛石英正长斑岩全岩含矿K-Ar36.0Hou et al., 2003c删除
      色礼二长花岗斑岩钾长石含矿K-Ar96.8刘荣谟和赵定华, 1981删除
      二长花岗斑岩锆石含矿LA U-Pb39.439.4陈喜连,2016
      吉错正长斑岩全岩含矿K-Ar40.7Hou et al., 2003c删除
      马牧普正长斑岩锆石含矿LA U-Pb38.538.5陈喜连,2016
      角闪石英正长斑岩全岩含矿Rb-Sr37.6Hou et al., 2003c删除
      巴达石英正长岩全岩不含矿K-Ar38.4Hou et al., 2003c删除
      总郭石英二长斑岩锆石含矿LA U-Pb39.439.4陈喜连,2016
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