Zircon U-Pb Geochronology of Ore-Bearing Porphyries in Baomai Deposit, Yulong Copper Belt, Tibet
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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.Abstract: Baomai porphyry copper-molybdenite deposit is an important part of the northern Yulong copper belt, Tibet, with typical porphyry-type mineralization and alteration. The latest exploration shows that both Cu and Mo resources have reached the medium-sized deposit, but the research work is still very poor. Based on the basic geological characteristics, intrusion ages of biotite granite porphyry and biotit-monzogranite are 41.3±0.2 Ma and 40.8±0.2 Ma, respectively, according to the LA-ICP-MS zircon U-Pb geochronology method. These results are consistent with those of Yulong and Zhanaga deposits. All of them are the products of continent collision orogeny of India with Eurasia in Eocene. Geochronology evidences show that porphyries related to mineralization in the Yulong copper belt are mainly intruded at 37-42 Ma, and no obviously early (51 Ma), medium (41 Ma) and late (33 Ma) stages magmatic activities. From northwest to southeast, the ages of diagenesis and mineralization in Yulong copper belt do not change to be younger significantly.
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图 1 西藏玉龙斑岩铜矿带区域构造位置
据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
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/U 207Pb/206Pb 1σ 207Pb/235U 1σ 206Pb/238U 1σ 206Pb/238U(Ma) 1σ 黑云母花岗岩 ZK0208-266.0 m-1 629 903 0.7 0.051 6 0.003 2 0.044 6 0.002 9 0.006 3 0.000 1 40.7 0.8 ZK0208-266.0 m-2 497 958 0.5 0.051 5 0.003 7 0.044 4 0.003 2 0.006 2 0.000 1 40.1 0.7 ZK0208-266.0 m-4 1 531 1 626 0.9 0.052 3 0.004 4 0.045 5 0.003 6 0.006 4 0.000 1 41.0 0.8 ZK0208-266.0 m-5 675 1 294 0.5 0.052 1 0.002 6 0.045 4 0.002 2 0.006 3 0.000 1 40.8 0.5 ZK0208-266.0 m-6 686 1 161 0.6 0.052 4 0.002 2 0.045 8 0.001 8 0.006 4 0.000 1 41.2 0.5 ZK0208-266.0 m-7 1 723 2 497 0.7 0.048 1 0.002 3 0.041 4 0.001 9 0.006 3 0.000 1 40.2 0.5 ZK0208-266.0 m-9 789 1 360 0.6 0.051 0 0.002 0 0.044 2 0.001 6 0.006 4 0.000 1 41.3 0.5 ZK0208-266.0 m-10 608 1 205 0.5 0.050 9 0.002 9 0.044 0 0.002 5 0.006 4 0.000 1 40.9 0.6 ZK0208-266.0 m-11 354 1 124 0.3 0.050 6 0.002 5 0.044 2 0.002 2 0.006 5 0.000 1 41.7 0.6 ZK0208-266.0 m-12 541 1 083 0.5 0.051 8 0.002 3 0.045 2 0.002 1 0.006 4 0.000 1 41.2 0.6 ZK0208-266.0 m-13 1 068 2 050 0.5 0.048 2 0.001 9 0.042 9 0.001 8 0.006 5 0.000 1 41.6 0.5 ZK0208-266.0 m-14 483 1 194 0.4 0.050 1 0.002 6 0.044 3 0.002 3 0.006 6 0.000 1 42.1 0.6 ZK0208-266.0 m-15 611 1 343 0.5 0.047 7 0.002 7 0.042 8 0.002 3 0.006 5 0.000 1 41.9 0.5 ZK0208-266.0 m-16 745 1 424 0.5 0.049 9 0.002 2 0.044 3 0.002 0 0.006 5 0.000 1 41.7 0.5 ZK0208-266.0 m-19 729 1 014 0.7 0.048 1 0.007 2 0.042 4 0.006 7 0.006 5 0.000 2 41.7 1.4 ZK0208-266.0 m-20 744 1 188 0.6 0.052 2 0.002 6 0.045 3 0.002 1 0.006 5 0.000 1 41.7 0.6 ZK0208-266.0 m-21 1 642 1 990 0.8 0.050 7 0.002 1 0.044 2 0.001 9 0.006 3 0.000 1 40.7 0.5 ZK0208-266.0 m-22 316 713 0.4 0.050 5 0.008 1 0.040 6 0.004 8 0.006 2 0.000 3 40.0 2.0 ZK0208-266.0 m-23 469 688 0.7 0.052 7 0.019 9 0.044 3 0.012 9 0.006 4 0.000 5 41.3 2.9 ZK0208-266.0 m-24 707 1 610 0.4 0.051 2 0.002 8 0.043 7 0.002 3 0.006 3 0.000 1 40.3 0.5 ZK0208-266.0 m-25 618 900 0.7 0.052 7 0.002 7 0.046 0 0.002 3 0.006 5 0.000 1 41.5 0.6 ZK0208-266.0 m-26 739 1 583 0.5 0.051 0 0.002 2 0.044 8 0.002 0 0.006 4 0.000 1 41.1 0.5 ZK0208-266.0 m-27 1 381 2 204 0.6 0.048 9 0.002 0 0.043 4 0.001 8 0.006 5 0.000 1 41.9 0.5 ZK0208-266.0 m-28 1 697 1 317 1.3 0.050 0 0.003 0 0.044 1 0.002 6 0.006 5 0.000 1 41.7 0.6 ZK0208-266.0 m-29 783 1 599 0.5 0.046 2 0.002 1 0.041 0 0.001 9 0.006 5 0.000 1 41.8 0.6 ZK0208-266.0 m-30 1 182 1 246 0.9 0.052 2 0.002 7 0.045 5 0.002 4 0.006 4 0.000 1 41.1 0.7 黑云母二长花岗岩 ZK0507-789.2 m-1 592 1 014 0.6 0.043 4 0.002 8 0.037 4 0.002 5 0.006 2 0.000 1 40.2 0.6 ZK0507-789.2 m-2 661 1 076 0.6 0.052 7 0.002 0 0.046 3 0.002 0 0.006 3 0.000 1 40.6 0.5 ZK0507-789.2 m-3 541 1 514 0.4 0.050 5 0.001 7 0.043 3 0.001 5 0.006 3 0.000 1 40.4 0.5 ZK0507-789.2 m-5 376 905 0.4 0.051 4 0.003 0 0.046 2 0.002 9 0.006 5 0.000 1 41.6 0.8 ZK0507-789.2 m-6 1 100 1 689 0.7 0.052 6 0.004 6 0.044 3 0.003 4 0.006 2 0.000 1 40.1 0.8 ZK0507-789.2 m-7 844 1 665 0.5 0.050 6 0.002 7 0.043 5 0.002 3 0.006 2 0.000 1 40.1 0.6 ZK0507-789.2 m-8 623 1 346 0.5 0.052 8 0.004 6 0.045 4 0.003 8 0.006 4 0.000 1 41.2 0.9 ZK0507-789.2 m-9 726 1 365 0.5 0.050 9 0.002 7 0.043 6 0.002 2 0.006 3 0.000 1 40.3 0.7 ZK0507-789.2 m-10 951 1 555 0.6 0.048 3 0.003 5 0.041 3 0.002 9 0.006 2 0.000 1 40.1 0.8 ZK0507-789.2 m-11 807 1 248 0.7 0.051 8 0.002 7 0.044 9 0.002 4 0.006 3 0.000 1 40.3 0.5 ZK0507-789.2 m-12 848 1 505 0.6 0.050 3 0.002 4 0.043 1 0.002 0 0.0063 0.000 1 40.3 0.5 ZK0507-789.2 m-13 648 1 437 0.5 0.048 5 0.002 1 0.042 4 0.001 8 0.006 4 0.000 1 40.9 0.5 ZK0507-789.2 m-14 746 1 125 0.7 0.051 3 0.002 1 0.044 6 0.001 8 0.006 4 0.000 1 41.0 0.5 ZK0507-789.2 m-15 1 002 1 648 0.6 0.051 2 0.001 9 0.045 3 0.001 7 0.006 4 0.000 1 41.2 0.5 ZK0507-789.2 m-16 712 1 481 0.5 0.050 2 0.002 0 0.043 8 0.001 9 0.006 4 0.000 1 41.2 0.6 ZK0507-789.2 m-17 629 1 586 0.4 0.050 7 0.002 2 0.043 2 0.001 8 0.006 2 0.000 1 40.0 0.5 ZK0507-789.2 m-18 872 1 444 0.6 0.049 1 0.002 1 0.042 5 0.001 8 0.0063 0.000 1 40.6 0.5 ZK0507-789.2 m-19 1 035 1 059 1.0 0.050 3 0.004 0 0.042 8 0.003 5 0.006 2 0.000 1 39.6 0.8 ZK0507-789.2 m-20 544 1 242 0.4 0.049 8 0.002 3 0.043 5 0.002 1 0.006 3 0.000 1 40.7 0.5 ZK0507-789.2 m-21 282 644 0.4 0.054 3 0.004 4 0.044 8 0.003 2 0.006 2 0.000 2 40.2 1.0 ZK0507-789.2 m-22 517 1 144 0.5 0.047 5 0.002 0 0.041 4 0.001 7 0.006 4 0.000 1 41.2 0.5 ZK0507-789.2 m-23 732 1 566 0.5 0.050 5 0.002 1 0.044 6 0.001 9 0.006 5 0.000 1 41.6 0.5 ZK0507-789.2 m-24 1 011 1 182 0.9 0.049 9 0.002 4 0.044 4 0.002 1 0.006 5 0.000 1 41.8 0.6 ZK0507-789.2 m-25 975 1 520 0.7 0.044 7 0.002 2 0.039 4 0.002 0 0.006 5 0.000 1 41.5 0.6 ZK0507-789.2 m-26 1 051 1 399 0.8 0.051 7 0.002 3 0.045 2 0.001 9 0.006 5 0.000 1 41.6 0.5 ZK0507-789.2 m-27 479 1 015 0.5 0.0521 0.002 6 0.045 8 0.002 1 0.006 5 0.000 1 41.7 0.6 ZK0507-789.2 m-28 920 1 407 0.7 0.049 6 0.002 0 0.043 5 0.001 8 0.006 4 0.000 1 41.1 0.5 ZK0507-789.2 m-29 993 1 292 0.8 0.051 5 0.002 3 0.043 8 0.001 9 0.006 3 0.000 1 40.3 0.5 ZK0507-789.2 m-30 606 1 049 0.6 0.051 1 0.004 8 0.045 6 0.004 1 0.006 5 0.000 2 41.9 1.2 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). 
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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、Mo Cu、Mo、Fe、As Cu、Mo、Fe、W、Au、Ag、Pb、Zn、Ni、Co Cu、Mo、Au、Fe Cu、Mo、Au、Ag Cu、Mo、Au、Ag、PGE Cu、Mo Cu、Au、Ag Cu 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.
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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-Os 40.8 40.9 郝金华等，2012 石英-辉钼矿脉 辉钼矿 矿化 Re-Os 40.9 王召林等，2008 黑云母花岗斑岩 锆石 含矿 LA U-Pb 43.4 42.3 郝金华等，2012 黑云母花岗斑岩 锆石 含矿 LA U-Pb 42.9 郝金华等，2012 黑云母花岗斑岩 锆石 含矿 LA U-Pb 41.5 宋忠宝等，2011 花岗闪长斑岩 锆石 含矿 LA U-Pb 41.4 宋忠宝等，2011 斜长花岗斑岩 锆石 含矿 LA U-Pb 41.0 宋忠宝等，2011 黑云母花岗斑岩 锆石 含矿 SHRIMP 43.3 杨志明等，2008 日胆果 二长花岗斑岩 长石 含矿 K-Ar 41.5 41.5 Hou et al., 2003c 参考 二长花岗斑岩 钾长石 含矿 K-Ar 41.5 Hou et al., 2003c 参考 夏日多 二长花岗斑岩 钾长石 无矿 K-Ar 46.0 马鸿文，1990 删除 包买 黑云母花岗岩 锆石 含矿 LA U-Pb 41.3 41.1 本文 黑云母二长花岗岩 锆石 含矿 LA U-Pb 40.8 本文 恒星错 花岗闪长岩 钾长石 含矿 K-Ar 40.7 刘荣谟和赵定华, 1981 参考 二长花岗斑岩 钾长石 含矿 K-Ar 41.5 41.3 唐仁鲤和罗怀松, 1995 参考 二长花岗斑岩 钾长石 含矿 K-Ar 41.0 唐仁鲤和罗怀松, 1995 参考 二长花岗斑岩 全岩 含矿 K-Ar 42.7 刘荣谟和赵定华, 1981 删除 玉龙 二长花岗斑岩 黑云母 含矿 K-Ar 40.7 马鸿文，1989b 删除 二长花岗斑岩 黑云母 含矿 K-Ar 48.2 马鸿文，1989b 删除 二长花岗斑岩 黑云母 含矿 K-Ar 41.5 刘荣谟和赵定华, 1981 删除 二长花岗斑岩 钾长石 含矿 K-Ar 40.0 刘荣谟和赵定华, 1981 删除 二长花岗斑岩 钾长石 含矿 K-Ar 37.9 刘荣谟和赵定华, 1981 删除 二长花岗斑岩 钾长石 含矿 K-Ar 38.2 刘荣谟和赵定华, 1981 删除 二长花岗斑岩 钾长石 含矿 K-Ar 55.0 马鸿文，1989b 删除 二长花岗斑岩 钾长石 含矿 K-Ar 55.0 马鸿文，1989b 删除 二长花岗斑岩 黑云母 含矿 Rb-Sr 41.0 马鸿文，1989b 删除 二长花岗斑岩 黑云母 含矿 Rb-Sr 41.0 马鸿文，1989b 删除 二长花岗斑岩 钾长石 含矿 K-Ar 38.0 张玉泉等，1987 删除 二长花岗斑岩 钾长石 含矿 K-Ar 41.0 张玉泉等，1987 删除 二长花岗斑岩 黑云母 含矿 Ar-Ar 52.8 马鸿文，1989b 删除 二长花岗斑岩 黑云母 含矿 Rb-Sr 52.0 马鸿文，1989b 删除 石英-辉钼矿脉 辉钼矿 含矿 Re-Os 40.1 40.9 曾普胜等，2006 石英-辉钼矿脉 辉钼矿 含矿 Re-Os 41.6 唐菊兴等，2009 石英二长花岗斑岩 锆石 成矿前 LA U-Pb 41.3 42.1 梁华英等，2008 含矿斑岩 锆石 含矿 LA U-Pb 41.2 Liang et al., 2006 二长花岗岩 锆石 含矿 SHRIMP 40.9 曾普胜等，2006 石英二长斑岩 锆石 成矿前 SHRIMP 43.6 郭利果等，2006 黑云母二长花岗斑岩 锆石 含矿 SHRIMP 41.0 郭利果等，2006 黑云母二长花岗斑岩 锆石 含矿 SHRIMP 43.8 王成辉等，2009 黑云母二长花岗斑岩 锆石 含矿 SHRIMP 43.0 王成辉等，2009 正长花岗斑岩 黑云母 含矿 Ar-Ar 41.7 梁华英等，2008 玉龙北甘龙拉 石英斜长斑岩 锆石 含矿 SHRIMP 43.9 王成辉等，2009 玉龙南纳加 石英二长花岗斑岩 锆石 无矿 SHRIMP 41.4 王成辉等，2009 扎那尕 二长花岗斑岩 黑云母 含矿 K-Ar 40.0 张玉泉等，1987 删除 二长花岗斑岩 钾长石 含矿 K-Ar 33.9 刘荣谟和赵定华, 1981 删除 二长花岗斑岩 钾长石 含矿 K-Ar 34.0 张玉泉等，1987 删除 含矿斑岩 锆石 含矿 LA U-Pb 38.5 38.5 Liang et al., 2006 莽总 二长花岗斑岩 钾长石 含矿 K-Ar 33.9 刘荣谟和赵定华, 1981 删除 二长花岗斑岩 锆石 含矿 LA U-Pb 37.6 37.6 Liang et al., 2006 二长花岗斑岩 钾长石 含矿 K-Ar 42.7 马鸿文等，1989b 删除 多霞松多 含矿斑岩 锆石 含矿 LA U-Pb 37.5 37.5 Liang et al., 2006 花岗斑岩 锆石 含矿 U-Pb 41.0 马鸿文等，1990 删除 二长花岗斑岩 全岩 含矿 Rb-Sr 52.0 马鸿文等，1990 删除 马拉松多 花岗斑岩 锆石 含矿 U-Pb 41.0 马鸿文等，1990 删除 正长花岗斑岩 钾长石 含矿 K-Ar 35.8 唐仁鲤和罗怀松, 1995 删除 二长花岗斑岩 锆石 含矿 U-Pb 40.9 马鸿文等，1990 删除 二长花岗斑岩 全岩 含矿 K-Ar 50.9 唐仁鲤等., 1995 删除 石英二长斑岩 锆石 成矿前 LA U-Pb 36.9 36.9 梁华英等，2009 碱长花岗斑岩 锆石 含矿 LA U-Pb 36.9 梁华英等，2009 碱长花岗斑岩 黑云母 含矿 K-Ar 36.9 梁华英等，2009 石英-辉钼矿脉 辉钼矿 含矿 Re-Os 35.9 35.8 唐仁鲤和罗怀松, 1995 石英-辉钼矿脉 辉钼矿 含矿 Re-Os 35.4 唐仁鲤和罗怀松, 1995 石英-辉钼矿脉 辉钼矿 含矿 Re-Os 36.2 唐仁鲤和罗怀松, 1995 石英-辉钼矿脉 辉钼矿 含矿 Re-Os 35.8 杜安道等，1994 拉日玛 石英正长斑岩 全岩 含矿 K-Ar 36.0 Hou et al., 2003c 删除 色礼 二长花岗斑岩 钾长石 含矿 K-Ar 96.8 刘荣谟和赵定华, 1981 删除 二长花岗斑岩 锆石 含矿 LA U-Pb 39.4 39.4 陈喜连，2016 吉错 正长斑岩 全岩 含矿 K-Ar 40.7 Hou et al., 2003c 删除 马牧普 正长斑岩 锆石 含矿 LA U-Pb 38.5 38.5 陈喜连，2016 角闪石英正长斑岩 全岩 含矿 Rb-Sr 37.6 Hou et al., 2003c 删除 巴达 石英正长岩 全岩 不含矿 K-Ar 38.4 Hou et al., 2003c 删除 总郭 石英二长斑岩 锆石 含矿 LA U-Pb 39.4 39.4 陈喜连，2016
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