现代地质 ›› 2018, Vol. 32 ›› Issue (02): 289-304.DOI: 10.19657/j.geoscience.1000-8527.2018.02.08
肖昌浩1,2(), 申玉科1(
), 韦昌山1, 苏晓凯1,2, 乐兴文3, 张亮2
收稿日期:
2017-07-12
修回日期:
2018-01-11
出版日期:
2018-04-10
发布日期:
2018-05-07
通讯作者:
申玉科,男,副研究员,1966年出生,地质力学专业,从事矿田构造研究工作。Email:yk_s705@126.com。
作者简介:
肖昌浩,男,助理研究员,1986年出生,矿床学与矿床地球化学专业,主要从事矿床学研究。 Email:xiaochanghao1986@126.com。
基金资助:
XIAO Changhao1,2(), SHEN Yuke1(
), WEI Changshan1, SU Xiaokai1,2, LE Xingwen3, ZHANG Liang2
Received:
2017-07-12
Revised:
2018-01-11
Online:
2018-04-10
Published:
2018-05-07
摘要:
广西西大明山多金属矿集区位于右江褶皱带东南缘。LA-ICP-MS锆石 U-Pb定年结果显示,区内那宁石英斑岩脉、罗维隐伏二长花岗岩和黑云母花岗岩岩体的侵位年龄分别为(93.11±0.64)Ma、(92.92±0.69)Ma和(92.5±1.1)Ma,说明三者都形成于晚白垩世。Hf同位素组成结果显示,石英斑岩中锆石εHf(t)值变化于-18.4~-1.2之间,两阶段模式年龄变化于1 236~2 326 Ma之间。二长花岗岩和黑云母花岗岩锆石εHf(t)值分别为-19.4~+0.3和-12.2~-3.6,两阶段模式年龄分别变化于1 139~2 385 Ma和1 386~1 933 Ma,表明它们主要来源于中元古代末期增生的地壳组分与少量古元古代地壳地质的共同熔融。通过与右江褶皱带周缘岩浆岩带锆石Hf同位素特征对比,认为右江褶皱带周缘岩浆岩可能具有一致的物源。二长花岗岩和黑云母花岗岩中锆石的Ce(IV)/Ce(Ⅲ)比值平均值分别为23.65和33.76,说明罗维隐伏岩体具有较低的氧逸度。通过对比右江褶皱带周缘前人的成矿年代学及同位素研究,显示该区成岩成矿时间较短(92~95 Ma),形成于晚白垩世区域伸展构造体制下,右江褶皱带岩石圈发生松弛和伸展垮塌,导致中元古代和少量古元古代地壳发生部分熔融,形成大规模岩浆作用。结合右江褶皱带周缘岩浆带大地构造位置及成岩时代,认为右江褶皱带燕山期岩浆岩的形成可能受到太平洋构造域和特提斯构造域双重作用,可能以后者为主。
中图分类号:
肖昌浩, 申玉科, 韦昌山, 苏晓凯, 乐兴文, 张亮. 广西右江褶皱带东南缘西大明山矿集区燕山期酸性岩浆锆石U-Pb年龄、Hf同位素和Ce(IV)/Ce(III)特征[J]. 现代地质, 2018, 32(02): 289-304.
XIAO Changhao, SHEN Yuke, WEI Changshan, SU Xiaokai, LE Xingwen, ZHANG Liang. LA-ICP-MS Zircon U-Pb Dating,Hf Isotopic Composition and Ce4+/Ce3+ Characteristics of the Yanshanian Acid Magma in the Xidamingshan Cluster,Southeastern Margin of the Youjiang Fold Belt,Guangxi[J]. Geoscience, 2018, 32(02): 289-304.
图1 广西西大明山矿集区地质简图及主要矿床、矿点分布图[3,20]
Fig.1 Geological sketch map of the Xidamingshan cluster, southeastern margin of the Youjiang fold belt,showing the distribution of main ore deposits
图2 西大明山矿集区燕山期花岗岩手标本及显微照片 Q.石英;Pl.斜长石;Ser.绢云母;Hbl.角闪石;Kfs.钾长石;Bt.黑云母;Mu.白云母
Fig. 2 Hand specimens and photomicrographs showing petro-logy of the Yanshanian magma in the Xidamingshancluster
图3 西大明山矿集区燕山期花岗岩代表性锆石阴极发光图像及测点位置、U-Pb年龄和εHf(t)值
Fig.3 Cathodoluminescence(CL)images of representative zircons of the Yanshanian magma in the Xidamingshan cluster,southeastern margin of the Youjiang fold belt with analytical numbers,U-Pb ages and εHf(t)
岩石 | 样号 | La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu | Th | U | Hf | Ce4+/Ce3+ | |||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
ZK 31901 黑 云 母 二 长 花 岗 岩 (LW 01) | LW01-01 | 0027.16 | 00428.11 | 0019.24 | 00132.85 | 00183.32 | 28.06 | 395.59 | 00125.08 | 1 388.57 | 478.92 | 1 936.7 | 472.92 | 4 343.8 | 0728.2 | 10 503.8 | 7 507.6 | 31 766.6 | 10.10 | |||||||||||||||||||
LW01-02 | 0.05 | 93.81 | 0.77 | 13.57 | 56.66 | 8.73 | 260.91 | 121.81 | 1 676.95 | 665.36 | 3 080.5 | 765.79 | 7 654.4 | 1 311.0 | 2 010.0 | 6 834.1 | 35 806.8 | 87.13 | ||||||||||||||||||||
LW01-03 | 99.44 | 713.79 | 45.90 | 239.99 | 224.47 | 24.75 | 514.17 | 167.61 | 1 795.72 | 596.17 | 2 404.6 | 532.78 | 4 773.7 | 782.6 | 9 782.1 | 6 035.7 | 27 848.9 | 8.02 | ||||||||||||||||||||
LW01-04 | 7.60 | 226.27 | 4.81 | 38.79 | 97.95 | 14.06 | 371.41 | 148.35 | 1 848.48 | 687.15 | 3 034.6 | 688.01 | 6 411.3 | 1 070.3 | 5 936.7 | 9 621.0 | 34 213.3 | 34.43 | ||||||||||||||||||||
LW01-05 | 48.29 | 823.44 | 31.48 | 252.79 | 332.64 | 41.82 | 841.67 | 264.89 | 2 798.96 | 907.18 | 3 661.1 | 781.32 | 6 998.3 | 1 153.6 | 14 011.8 | 6 960.3 | 26 947.0 | 11.10 | ||||||||||||||||||||
LW01-06 | 7.69 | 42.77 | 5.01 | 33.90 | 81.77 | 5.36 | 294.85 | 115.12 | 1 369.88 | 491.52 | 2 174.0 | 509.49 | 4 935.9 | 845.8 | 2 141.4 | 7 180.8 | 35 462.7 | 6.48 | ||||||||||||||||||||
LW01-07 | 36.76 | 48.61 | 20.55 | 65.44 | 52.09 | 3.43 | 200.65 | 86.29 | 1 232.81 | 476.63 | 2 263.7 | 583.92 | 5 962.0 | 1 086.5 | 1 296.7 | 12 055.4 | 36 178.2 | 2.92 | ||||||||||||||||||||
LW01-08 | 0.00 | 24.66 | 0.78 | 19.16 | 76.06 | 2.83 | 331.33 | 147.47 | 1 862.69 | 703.38 | 3 162.6 | 752.75 | 7 322.7 | 1 229.2 | 3 158.4 | 12 950.5 | 34 385.0 | 20.38 | ||||||||||||||||||||
LW01-09 | 1.59 | 95.61 | 1.66 | 16.35 | 54.44 | 4.24 | 270.82 | 110.33 | 1 512.45 | 556.65 | 2 531.1 | 635.86 | 6 233.4 | 1 092.5 | 2 817.6 | 12 751.9 | 35 852.4 | 54.36 | ||||||||||||||||||||
LW01-10 | 5.45 | 511.16 | 11.90 | 71.30 | 134.51 | 21.37 | 490.27 | 161.96 | 1 967.96 | 706.90 | 3 077.4 | 725.47 | 7 097.5 | 1 189.8 | 8 150.5 | 9 980.8 | 23 306.7 | 31.14 | ||||||||||||||||||||
LW01-11 | 16.82 | 173.91 | 177.43 | 406.76 | 173.53 | 22.60 | 394.46 | 160.50 | 1 856.22 | 615.61 | 2 677.9 | 674.76 | 6 687.3 | 1 118.4 | 2 973.2 | 12 428.5 | 36 338.5 | 0.01 | ||||||||||||||||||||
LW01-12 | 7.74 | 76.87 | 5.87 | 36.29 | 71.00 | 9.58 | 286.99 | 136.22 | 1 844.75 | 721.98 | 3 518.2 | 899.45 | 9 388.4 | 1 606.5 | 2 828.0 | 18 094.5 | 36 784.7 | 14.11 | ||||||||||||||||||||
LW01-13 | 700.12 | 548.01 | 198.27 | 447.84 | 193.95 | 13.40 | 406.88 | 154.69 | 1 956.39 | 709.34 | 3 295.3 | 858.08 | 8 954.9 | 1 483.1 | 5 157.2 | 21 641.3 | 35 534.9 | 2.52 | ||||||||||||||||||||
LW01-14 | 0.28 | 56.79 | 5.44 | 30.38 | 49.41 | 5.12 | 288.93 | 137.40 | 1 865.43 | 713.80 | 3 379.6 | 863.32 | 8 580.7 | 1 506.1 | 2 956.1 | 18 572.6 | 37 037.4 | 13.86 | ||||||||||||||||||||
LW01-15 | 0.28 | 62.38 | 11.36 | 44.98 | 52.70 | 8.12 | 253.48 | 118.55 | 1 584.67 | 592.07 | 2 760.8 | 731.11 | 7 475.3 | 1 298.8 | 2 234.5 | 14 034.0 | 38 518.1 | 6.72 | ||||||||||||||||||||
LW01-16 | 1.07 | 72.97 | 1.64 | 20.26 | 56.20 | 3.56 | 262.70 | 104.38 | 1 344.37 | 488.45 | 2 152.6 | 527.15 | 5 286.8 | 856.3 | 3 512.4 | 10 239.3 | 32 657.3 | 35.26 | ||||||||||||||||||||
LW01-17 | 0.82 | 42.41 | 1.23 | 10.04 | 54.40 | 5.37 | 283.15 | 124.01 | 1 733.54 | 656.99 | 3 074.5 | 782.41 | 8 217.6 | 1 371.3 | 2 869.4 | 18 443.9 | 34 118.6 | 37.61 | ||||||||||||||||||||
LW01-18 | 13.53 | 105.87 | 19.99 | 233.68 | 139.42 | 11.09 | 344.48 | 124.42 | 1 558.65 | 545.69 | 2 478.1 | 612.88 | 6 105.6 | 987.3 | 3 739.5 | 12 842.1 | 36 068.4 | 2.08 | ||||||||||||||||||||
LW01-19 | 1.69 | 152.04 | 1.85 | 30.35 | 60.10 | 7.69 | 293.31 | 118.65 | 1 587.83 | 589.00 | 2 728.1 | 735.42 | 7 811.3 | 1 271.6 | 3 969.7 | 23 067.4 | 36 131.0 | 58.62 | ||||||||||||||||||||
LW01-20 | 8 526.42 | 11 860.42 | 2 631.27 | 17 058.74 | 2 451.30 | 85.22 | 1 445.75 | 223.79 | 1 992.83 | 637.73 | 2 810.1 | 717.06 | 7 402.3 | 1 213.8 | 14 059.2 | 15 165.2 | 34 053.8 | 0.15 | ||||||||||||||||||||
LW01-21 | 4.71 | 582.12 | 12.53 | 168.69 | 136.75 | 28.51 | 484.92 | 154.12 | 1 909.19 | 685.73 | 2 964.1 | 723.13 | 6 874.3 | 1 084.0 | 22 960.8 | 15 163.7 | 31 754.1 | 21.73 | ||||||||||||||||||||
LW01-22 | 6.01 | 140.59 | 5.29 | 69.24 | 71.23 | 8.40 | 303.04 | 105.23 | 1 332.38 | 483.72 | 2 113.0 | 516.11 | 5 027.7 | 855.9 | 4 127.1 | 6 838.5 | 33 943.7 | 15.81 | ||||||||||||||||||||
LW01-23 | 1 865.41 | 2 448.07 | 529.37 | 3 533.15 | 515.60 | 25.87 | 454.26 | 130.78 | 1 721.71 | 659.86 | 3 205.2 | 868.32 | 9 225.5 | 1 592.1 | 2 460.3 | 16 085.1 | 41 641.7 | 1.71 | ||||||||||||||||||||
LW01-24 | 8.15 | 770.05 | 22.31 | 311.92 | 277.28 | 55.74 | 859.86 | 247.71 | 2 663.81 | 820.15 | 3 341.2 | 732.01 | 6 840.0 | 1 118.8 | 23 183.2 | 12 706.4 | 25 874.6 | 10.96 | ||||||||||||||||||||
LW01-25 | 0.01 | 27.59 | 0.21 | 4.74 | 25.16 | 4.61 | 177.68 | 80.66 | 1 194.30 | 465.37 | 2 259.4 | 615.69 | 6 396.6 | 1 081.8 | 1 516.9 | 15 314.1 | 40 069.4 | 104.54 | ||||||||||||||||||||
LW01-26 | 11.85 | 408.19 | 11.72 | 257.15 | 297.53 | 64.74 | 1 015.92 | 277.00 | 3 071.22 | 1 021.24 | 3 945.1 | 865.58 | 7 832.9 | 1 220.4 | 9 135.0 | 6 739.7 | 25 538.2 | 9.13 | ||||||||||||||||||||
LW01-27 | 6.56 | 807.51 | 7.05 | 168.59 | 209.31 | 36.83 | 744.08 | 209.22 | 2 286.04 | 741.82 | 2 929.2 | 636.32 | 5 828.6 | 931.2 | 15 972.1 | 6 895.3 | 28 000.7 | 33.13 | ||||||||||||||||||||
LW01-28 | 20.36 | 260.41 | 7.79 | 89.92 | 92.45 | 12.95 | 340.28 | 108.55 | 1 241.45 | 444.30 | 1 880.1 | 411.68 | 3 876.2 | 631.5 | 4 233.7 | 3 604.2 | 29 688.3 | 16.39 | ||||||||||||||||||||
LW01-29 | 264.11 | 422.92 | 78.38 | 546.18 | 115.45 | 10.98 | 291.32 | 115.38 | 1 608.98 | 632.21 | 3 073.9 | 812.80 | 8 490.2 | 1 453.0 | 2 898.3 | 20 737.4 | 36 513.8 | 3.96 | ||||||||||||||||||||
LW01-30 | 2.00 | 504.65 | 27.39 | 112.91 | 108.75 | 17.43 | 406.84 | 142.90 | 1 633.34 | 551.09 | 2 224.7 | 509.36 | 4 639.3 | 772.4 | 9 163.0 | 7 044.3 | 30 628.9 | 13.96 | ||||||||||||||||||||
LW01-31 | 0.54 | 43.68 | 8.46 | 28.81 | 36.51 | 3.88 | 215.18 | 98.66 | 1 445.22 | 531.80 | 2 533.5 | 672.89 | 6 490.5 | 1 202.3 | 1 559.2 | 13 970.1 | 38 294.0 | 8.28 | ||||||||||||||||||||
LW01-32 | 0.24 | 22.66 | 4.36 | 20.13 | 33.73 | 4.39 | 188.96 | 92.94 | 1 290.05 | 495.17 | 2 445.6 | 630.94 | 6 465.8 | 1 171.6 | 1 168.4 | 9 677.9 | 36 203.4 | 7.08 | ||||||||||||||||||||
岩石 | 样号 | La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu | Th | U | Hf | Ce4+/Ce3+ | |||||||||||||||||||
ZK 40004 黑 云 母 二 长 花 岗 岩 (LW15) | LW15-03 | 1.00 | 22.20 | 4.62 | 19.63 | 36.46 | 2.84 | 212.37 | 108.05 | 1 552.93 | 605.91 | 2 958.6 | 794.08 | 8 117.4 | 1 369.5 | 966.3 | 15 261.4 | 36 552.5 | 11.05 | |||||||||||||||||||
LW15-04 | 0.78 | 67.13 | 5.10 | 30.22 | 72.52 | 8.25 | 303.46 | 124.36 | 1 553.71 | 564.85 | 2 589.1 | 642.98 | 6 314.7 | 1 053.1 | 2 066.1 | 7 001.9 | 32 906.9 | 16.33 | ||||||||||||||||||||
LW15-06 | 1.26 | 186.78 | 7.14 | 52.08 | 109.34 | 15.72 | 405.72 | 144.58 | 1 658.53 | 557.06 | 2 337.8 | 543.47 | 4 865.8 | 811.6 | 4 451.4 | 6 372.3 | 31 334.2 | 21.50 | ||||||||||||||||||||
LW15-07 | 0.02 | 36.00 | 3.13 | 34.74 | 69.92 | 5.19 | 269.66 | 91.00 | 1 083.49 | 371.05 | 1 541.6 | 353.81 | 3 115.0 | 536.7 | 1 211.1 | 1 870.5 | 29 407.5 | 8.26 | ||||||||||||||||||||
LW15-08 | 0.06 | 17.20 | 0.96 | 11.19 | 40.90 | 3.64 | 216.95 | 107.59 | 1 489.26 | 573.84 | 2 791.8 | 723.90 | 7 375.9 | 1 268.4 | 1 088.5 | 9 549.5 | 36 361.7 | 24.49 | ||||||||||||||||||||
LW15-10 | 2.68 | 1 167.88 | 30.90 | 204.84 | 299.05 | 64.06 | 676.29 | 178.13 | 1 737.51 | 549.01 | 2 179.0 | 515.18 | 4 865.3 | 817.5 | 25 291.3 | 11 568.0 | 31 599.8 | 18.44 | ||||||||||||||||||||
LW15-11 | 0.14 | 191.45 | 11.36 | 84.77 | 149.21 | 27.04 | 483.49 | 167.02 | 1 926.50 | 632.94 | 2 695.4 | 588.49 | 5 328.3 | 901.9 | 2 742.0 | 2 113.8 | 26 034.1 | 11.60 | ||||||||||||||||||||
LW15-12 | 0.14 | 605.50 | 10.22 | 89.06 | 169.76 | 27.74 | 585.93 | 194.08 | 2 215.99 | 706.32 | 2 969.7 | 669.14 | 5 908.4 | 977.9 | 8 616.9 | 5 359.8 | 28 701.5 | 40.44 | ||||||||||||||||||||
LW15-13 | 0.02 | 19.99 | 0.27 | 4.79 | 26.80 | 3.69 | 180.82 | 98.18 | 1 474.81 | 598.49 | 3 036.6 | 851.58 | 8 785.1 | 1 555.3 | 1 018.1 | 15 955.4 | 36 749.2 | 104.60 | ||||||||||||||||||||
LW15-15 | 0.08 | 913.51 | 11.98 | 104.97 | 216.49 | 32.22 | 718.06 | 232.82 | 2 554.73 | 837.70 | 3 347.0 | 780.07 | 7 009.3 | 1 113.6 | 18 308.6 | 10 052.4 | 30 625.8 | 50.71 | ||||||||||||||||||||
LW15-16 | 3.00 | 39.83 | 5.47 | 10.75 | 31.39 | 4.19 | 192.61 | 96.44 | 1 373.91 | 536.28 | 2 636.7 | 689.62 | 7 146.6 | 1 206.5 | 1 130.2 | 12 011.1 | 36 348.0 | 22.47 | ||||||||||||||||||||
LW15-18 | 0.00 | 36.45 | 0.51 | 8.46 | 47.37 | 5.69 | 264.48 | 132.39 | 1 879.18 | 737.83 | 3 645.1 | 980.88 | 9 838.5 | 1 693.7 | 2 055.3 | 18 270.2 | 34 614.3 | 86.63 | ||||||||||||||||||||
LW15-21 | 1.06 | 633.90 | 14.75 | 96.18 | 159.23 | 29.67 | 506.78 | 168.02 | 1 881.10 | 629.31 | 2 634.6 | 628.09 | 5 887.2 | 939.2 | 12 341.2 | 9 754.4 | 28 133.8 | 32.78 |
表1 西大明山矿集区燕山期岩浆岩锆石微量元素含量
Table 1 Trace elements data for the zircons of the Yanshanian magma in the Xidamingshan cluster
岩石 | 样号 | La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu | Th | U | Hf | Ce4+/Ce3+ | |||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
ZK 31901 黑 云 母 二 长 花 岗 岩 (LW 01) | LW01-01 | 0027.16 | 00428.11 | 0019.24 | 00132.85 | 00183.32 | 28.06 | 395.59 | 00125.08 | 1 388.57 | 478.92 | 1 936.7 | 472.92 | 4 343.8 | 0728.2 | 10 503.8 | 7 507.6 | 31 766.6 | 10.10 | |||||||||||||||||||
LW01-02 | 0.05 | 93.81 | 0.77 | 13.57 | 56.66 | 8.73 | 260.91 | 121.81 | 1 676.95 | 665.36 | 3 080.5 | 765.79 | 7 654.4 | 1 311.0 | 2 010.0 | 6 834.1 | 35 806.8 | 87.13 | ||||||||||||||||||||
LW01-03 | 99.44 | 713.79 | 45.90 | 239.99 | 224.47 | 24.75 | 514.17 | 167.61 | 1 795.72 | 596.17 | 2 404.6 | 532.78 | 4 773.7 | 782.6 | 9 782.1 | 6 035.7 | 27 848.9 | 8.02 | ||||||||||||||||||||
LW01-04 | 7.60 | 226.27 | 4.81 | 38.79 | 97.95 | 14.06 | 371.41 | 148.35 | 1 848.48 | 687.15 | 3 034.6 | 688.01 | 6 411.3 | 1 070.3 | 5 936.7 | 9 621.0 | 34 213.3 | 34.43 | ||||||||||||||||||||
LW01-05 | 48.29 | 823.44 | 31.48 | 252.79 | 332.64 | 41.82 | 841.67 | 264.89 | 2 798.96 | 907.18 | 3 661.1 | 781.32 | 6 998.3 | 1 153.6 | 14 011.8 | 6 960.3 | 26 947.0 | 11.10 | ||||||||||||||||||||
LW01-06 | 7.69 | 42.77 | 5.01 | 33.90 | 81.77 | 5.36 | 294.85 | 115.12 | 1 369.88 | 491.52 | 2 174.0 | 509.49 | 4 935.9 | 845.8 | 2 141.4 | 7 180.8 | 35 462.7 | 6.48 | ||||||||||||||||||||
LW01-07 | 36.76 | 48.61 | 20.55 | 65.44 | 52.09 | 3.43 | 200.65 | 86.29 | 1 232.81 | 476.63 | 2 263.7 | 583.92 | 5 962.0 | 1 086.5 | 1 296.7 | 12 055.4 | 36 178.2 | 2.92 | ||||||||||||||||||||
LW01-08 | 0.00 | 24.66 | 0.78 | 19.16 | 76.06 | 2.83 | 331.33 | 147.47 | 1 862.69 | 703.38 | 3 162.6 | 752.75 | 7 322.7 | 1 229.2 | 3 158.4 | 12 950.5 | 34 385.0 | 20.38 | ||||||||||||||||||||
LW01-09 | 1.59 | 95.61 | 1.66 | 16.35 | 54.44 | 4.24 | 270.82 | 110.33 | 1 512.45 | 556.65 | 2 531.1 | 635.86 | 6 233.4 | 1 092.5 | 2 817.6 | 12 751.9 | 35 852.4 | 54.36 | ||||||||||||||||||||
LW01-10 | 5.45 | 511.16 | 11.90 | 71.30 | 134.51 | 21.37 | 490.27 | 161.96 | 1 967.96 | 706.90 | 3 077.4 | 725.47 | 7 097.5 | 1 189.8 | 8 150.5 | 9 980.8 | 23 306.7 | 31.14 | ||||||||||||||||||||
LW01-11 | 16.82 | 173.91 | 177.43 | 406.76 | 173.53 | 22.60 | 394.46 | 160.50 | 1 856.22 | 615.61 | 2 677.9 | 674.76 | 6 687.3 | 1 118.4 | 2 973.2 | 12 428.5 | 36 338.5 | 0.01 | ||||||||||||||||||||
LW01-12 | 7.74 | 76.87 | 5.87 | 36.29 | 71.00 | 9.58 | 286.99 | 136.22 | 1 844.75 | 721.98 | 3 518.2 | 899.45 | 9 388.4 | 1 606.5 | 2 828.0 | 18 094.5 | 36 784.7 | 14.11 | ||||||||||||||||||||
LW01-13 | 700.12 | 548.01 | 198.27 | 447.84 | 193.95 | 13.40 | 406.88 | 154.69 | 1 956.39 | 709.34 | 3 295.3 | 858.08 | 8 954.9 | 1 483.1 | 5 157.2 | 21 641.3 | 35 534.9 | 2.52 | ||||||||||||||||||||
LW01-14 | 0.28 | 56.79 | 5.44 | 30.38 | 49.41 | 5.12 | 288.93 | 137.40 | 1 865.43 | 713.80 | 3 379.6 | 863.32 | 8 580.7 | 1 506.1 | 2 956.1 | 18 572.6 | 37 037.4 | 13.86 | ||||||||||||||||||||
LW01-15 | 0.28 | 62.38 | 11.36 | 44.98 | 52.70 | 8.12 | 253.48 | 118.55 | 1 584.67 | 592.07 | 2 760.8 | 731.11 | 7 475.3 | 1 298.8 | 2 234.5 | 14 034.0 | 38 518.1 | 6.72 | ||||||||||||||||||||
LW01-16 | 1.07 | 72.97 | 1.64 | 20.26 | 56.20 | 3.56 | 262.70 | 104.38 | 1 344.37 | 488.45 | 2 152.6 | 527.15 | 5 286.8 | 856.3 | 3 512.4 | 10 239.3 | 32 657.3 | 35.26 | ||||||||||||||||||||
LW01-17 | 0.82 | 42.41 | 1.23 | 10.04 | 54.40 | 5.37 | 283.15 | 124.01 | 1 733.54 | 656.99 | 3 074.5 | 782.41 | 8 217.6 | 1 371.3 | 2 869.4 | 18 443.9 | 34 118.6 | 37.61 | ||||||||||||||||||||
LW01-18 | 13.53 | 105.87 | 19.99 | 233.68 | 139.42 | 11.09 | 344.48 | 124.42 | 1 558.65 | 545.69 | 2 478.1 | 612.88 | 6 105.6 | 987.3 | 3 739.5 | 12 842.1 | 36 068.4 | 2.08 | ||||||||||||||||||||
LW01-19 | 1.69 | 152.04 | 1.85 | 30.35 | 60.10 | 7.69 | 293.31 | 118.65 | 1 587.83 | 589.00 | 2 728.1 | 735.42 | 7 811.3 | 1 271.6 | 3 969.7 | 23 067.4 | 36 131.0 | 58.62 | ||||||||||||||||||||
LW01-20 | 8 526.42 | 11 860.42 | 2 631.27 | 17 058.74 | 2 451.30 | 85.22 | 1 445.75 | 223.79 | 1 992.83 | 637.73 | 2 810.1 | 717.06 | 7 402.3 | 1 213.8 | 14 059.2 | 15 165.2 | 34 053.8 | 0.15 | ||||||||||||||||||||
LW01-21 | 4.71 | 582.12 | 12.53 | 168.69 | 136.75 | 28.51 | 484.92 | 154.12 | 1 909.19 | 685.73 | 2 964.1 | 723.13 | 6 874.3 | 1 084.0 | 22 960.8 | 15 163.7 | 31 754.1 | 21.73 | ||||||||||||||||||||
LW01-22 | 6.01 | 140.59 | 5.29 | 69.24 | 71.23 | 8.40 | 303.04 | 105.23 | 1 332.38 | 483.72 | 2 113.0 | 516.11 | 5 027.7 | 855.9 | 4 127.1 | 6 838.5 | 33 943.7 | 15.81 | ||||||||||||||||||||
LW01-23 | 1 865.41 | 2 448.07 | 529.37 | 3 533.15 | 515.60 | 25.87 | 454.26 | 130.78 | 1 721.71 | 659.86 | 3 205.2 | 868.32 | 9 225.5 | 1 592.1 | 2 460.3 | 16 085.1 | 41 641.7 | 1.71 | ||||||||||||||||||||
LW01-24 | 8.15 | 770.05 | 22.31 | 311.92 | 277.28 | 55.74 | 859.86 | 247.71 | 2 663.81 | 820.15 | 3 341.2 | 732.01 | 6 840.0 | 1 118.8 | 23 183.2 | 12 706.4 | 25 874.6 | 10.96 | ||||||||||||||||||||
LW01-25 | 0.01 | 27.59 | 0.21 | 4.74 | 25.16 | 4.61 | 177.68 | 80.66 | 1 194.30 | 465.37 | 2 259.4 | 615.69 | 6 396.6 | 1 081.8 | 1 516.9 | 15 314.1 | 40 069.4 | 104.54 | ||||||||||||||||||||
LW01-26 | 11.85 | 408.19 | 11.72 | 257.15 | 297.53 | 64.74 | 1 015.92 | 277.00 | 3 071.22 | 1 021.24 | 3 945.1 | 865.58 | 7 832.9 | 1 220.4 | 9 135.0 | 6 739.7 | 25 538.2 | 9.13 | ||||||||||||||||||||
LW01-27 | 6.56 | 807.51 | 7.05 | 168.59 | 209.31 | 36.83 | 744.08 | 209.22 | 2 286.04 | 741.82 | 2 929.2 | 636.32 | 5 828.6 | 931.2 | 15 972.1 | 6 895.3 | 28 000.7 | 33.13 | ||||||||||||||||||||
LW01-28 | 20.36 | 260.41 | 7.79 | 89.92 | 92.45 | 12.95 | 340.28 | 108.55 | 1 241.45 | 444.30 | 1 880.1 | 411.68 | 3 876.2 | 631.5 | 4 233.7 | 3 604.2 | 29 688.3 | 16.39 | ||||||||||||||||||||
LW01-29 | 264.11 | 422.92 | 78.38 | 546.18 | 115.45 | 10.98 | 291.32 | 115.38 | 1 608.98 | 632.21 | 3 073.9 | 812.80 | 8 490.2 | 1 453.0 | 2 898.3 | 20 737.4 | 36 513.8 | 3.96 | ||||||||||||||||||||
LW01-30 | 2.00 | 504.65 | 27.39 | 112.91 | 108.75 | 17.43 | 406.84 | 142.90 | 1 633.34 | 551.09 | 2 224.7 | 509.36 | 4 639.3 | 772.4 | 9 163.0 | 7 044.3 | 30 628.9 | 13.96 | ||||||||||||||||||||
LW01-31 | 0.54 | 43.68 | 8.46 | 28.81 | 36.51 | 3.88 | 215.18 | 98.66 | 1 445.22 | 531.80 | 2 533.5 | 672.89 | 6 490.5 | 1 202.3 | 1 559.2 | 13 970.1 | 38 294.0 | 8.28 | ||||||||||||||||||||
LW01-32 | 0.24 | 22.66 | 4.36 | 20.13 | 33.73 | 4.39 | 188.96 | 92.94 | 1 290.05 | 495.17 | 2 445.6 | 630.94 | 6 465.8 | 1 171.6 | 1 168.4 | 9 677.9 | 36 203.4 | 7.08 | ||||||||||||||||||||
岩石 | 样号 | La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu | Th | U | Hf | Ce4+/Ce3+ | |||||||||||||||||||
ZK 40004 黑 云 母 二 长 花 岗 岩 (LW15) | LW15-03 | 1.00 | 22.20 | 4.62 | 19.63 | 36.46 | 2.84 | 212.37 | 108.05 | 1 552.93 | 605.91 | 2 958.6 | 794.08 | 8 117.4 | 1 369.5 | 966.3 | 15 261.4 | 36 552.5 | 11.05 | |||||||||||||||||||
LW15-04 | 0.78 | 67.13 | 5.10 | 30.22 | 72.52 | 8.25 | 303.46 | 124.36 | 1 553.71 | 564.85 | 2 589.1 | 642.98 | 6 314.7 | 1 053.1 | 2 066.1 | 7 001.9 | 32 906.9 | 16.33 | ||||||||||||||||||||
LW15-06 | 1.26 | 186.78 | 7.14 | 52.08 | 109.34 | 15.72 | 405.72 | 144.58 | 1 658.53 | 557.06 | 2 337.8 | 543.47 | 4 865.8 | 811.6 | 4 451.4 | 6 372.3 | 31 334.2 | 21.50 | ||||||||||||||||||||
LW15-07 | 0.02 | 36.00 | 3.13 | 34.74 | 69.92 | 5.19 | 269.66 | 91.00 | 1 083.49 | 371.05 | 1 541.6 | 353.81 | 3 115.0 | 536.7 | 1 211.1 | 1 870.5 | 29 407.5 | 8.26 | ||||||||||||||||||||
LW15-08 | 0.06 | 17.20 | 0.96 | 11.19 | 40.90 | 3.64 | 216.95 | 107.59 | 1 489.26 | 573.84 | 2 791.8 | 723.90 | 7 375.9 | 1 268.4 | 1 088.5 | 9 549.5 | 36 361.7 | 24.49 | ||||||||||||||||||||
LW15-10 | 2.68 | 1 167.88 | 30.90 | 204.84 | 299.05 | 64.06 | 676.29 | 178.13 | 1 737.51 | 549.01 | 2 179.0 | 515.18 | 4 865.3 | 817.5 | 25 291.3 | 11 568.0 | 31 599.8 | 18.44 | ||||||||||||||||||||
LW15-11 | 0.14 | 191.45 | 11.36 | 84.77 | 149.21 | 27.04 | 483.49 | 167.02 | 1 926.50 | 632.94 | 2 695.4 | 588.49 | 5 328.3 | 901.9 | 2 742.0 | 2 113.8 | 26 034.1 | 11.60 | ||||||||||||||||||||
LW15-12 | 0.14 | 605.50 | 10.22 | 89.06 | 169.76 | 27.74 | 585.93 | 194.08 | 2 215.99 | 706.32 | 2 969.7 | 669.14 | 5 908.4 | 977.9 | 8 616.9 | 5 359.8 | 28 701.5 | 40.44 | ||||||||||||||||||||
LW15-13 | 0.02 | 19.99 | 0.27 | 4.79 | 26.80 | 3.69 | 180.82 | 98.18 | 1 474.81 | 598.49 | 3 036.6 | 851.58 | 8 785.1 | 1 555.3 | 1 018.1 | 15 955.4 | 36 749.2 | 104.60 | ||||||||||||||||||||
LW15-15 | 0.08 | 913.51 | 11.98 | 104.97 | 216.49 | 32.22 | 718.06 | 232.82 | 2 554.73 | 837.70 | 3 347.0 | 780.07 | 7 009.3 | 1 113.6 | 18 308.6 | 10 052.4 | 30 625.8 | 50.71 | ||||||||||||||||||||
LW15-16 | 3.00 | 39.83 | 5.47 | 10.75 | 31.39 | 4.19 | 192.61 | 96.44 | 1 373.91 | 536.28 | 2 636.7 | 689.62 | 7 146.6 | 1 206.5 | 1 130.2 | 12 011.1 | 36 348.0 | 22.47 | ||||||||||||||||||||
LW15-18 | 0.00 | 36.45 | 0.51 | 8.46 | 47.37 | 5.69 | 264.48 | 132.39 | 1 879.18 | 737.83 | 3 645.1 | 980.88 | 9 838.5 | 1 693.7 | 2 055.3 | 18 270.2 | 34 614.3 | 86.63 | ||||||||||||||||||||
LW15-21 | 1.06 | 633.90 | 14.75 | 96.18 | 159.23 | 29.67 | 506.78 | 168.02 | 1 881.10 | 629.31 | 2 634.6 | 628.09 | 5 887.2 | 939.2 | 12 341.2 | 9 754.4 | 28 133.8 | 32.78 |
岩石 | 点号 | 含量/10-6 | Th/U | 同位素比值 | 年龄/Ma | 谐和度 /% | ||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Pb | Th | U | 207Pb/206Pb | σ | 207Pb/235U | σ | 206Pb/238U | σ | 207Pb/235U | σ | 206Pb/238U | σ | 208Pb/232Th | σ | ||||||||||
那宁 石英 斑岩 (NN02), (93.11± 0.64) Ma, MSWD =1.04 | NN02-04 | 262 | 3 018 | 26 253 | 0.11 | 0.048 35 | 0.000 70 | 0.098 30 | 0.001 72 | 0.014 76 | 0.000 23 | 95.21 | 1.6 | 94.46 | 1.4 | 85.24 | 1.6 | 99 | ||||||
NN02-06 | 174 | 3 710 | 11 378 | 0.33 | 0.047 89 | 0.000 74 | 0.095 51 | 0.001 57 | 0.014 43 | 0.000 15 | 92.63 | 1.5 | 92.36 | 1.0 | 90.09 | 1.6 | 99 | |||||||
NN02-10 | 229 | 4 216 | 16 162 | 0.26 | 0.049 07 | 0.000 85 | 0.098 83 | 0.002 22 | 0.014 60 | 0.000 22 | 95.70 | 2.1 | 93.42 | 1.4 | 96.02 | 1.5 | 97 | |||||||
NN02-11 | 183 | 2 570 | 16 400 | 0.16 | 0.047 06 | 0.000 83 | 0.093 49 | 0.001 59 | 0.014 43 | 0.000 14 | 90.75 | 1.5 | 92.34 | 0.9 | 98.57 | 2.2 | 98 | |||||||
NN02-19 | 159 | 1 942 | 14 314 | 0.14 | 0.048 16 | 0.000 85 | 0.097 77 | 0.001 90 | 0.014 71 | 0.000 16 | 94.72 | 1.8 | 94.14 | 1.0 | 98.93 | 2.0 | 99 | |||||||
NN02-21 | 128 | 2 541 | 8 659 | 0.29 | 0.046 33 | 0.000 94 | 0.094 65 | 0.001 77 | 0.014 71 | 0.000 18 | 91.82 | 1.6 | 94.12 | 1.2 | 91.49 | 1.5 | 97 | |||||||
NN02-23 | 170 | 3 909 | 10 604 | 0.37 | 0.049 08 | 0.000 81 | 0.099 97 | 0.001 70 | 0.014 77 | 0.000 15 | 96.75 | 1.6 | 94.52 | 1.0 | 86.66 | 1.5 | 97 | |||||||
NN02-26 | 416 | 10 862 | 21 164 | 0.51 | 0.047 76 | 0.000 82 | 0.096 05 | 0.001 76 | 0.014 53 | 0.000 14 | 93.12 | 1.6 | 92.97 | 0.9 | 83.24 | 1.4 | 99 | |||||||
NN02-20 | 304 | 2 602 | 27 852 | 0.09 | 0.052 11 | 0.000 85 | 0.104 61 | 0.001 99 | 0.014 52 | 0.000 15 | 101.02 | 1.8 | 92.91 | 1.0 | 142.13 | 6.2 | 91 | |||||||
NN02-14 | 65 | 1 450 | 3 247 | 0.45 | 0.049 64 | 0.001 34 | 0.097 43 | 0.002 65 | 0.014 28 | 0.000 15 | 94.40 | 2.5 | 91.38 | 1.0 | 94.57 | 1.9 | 96 | |||||||
岩石 | 点号 | 含量/10-6 | Th/U | 同位素比值 | 年龄/Ma | 谐和度 /% | ||||||||||||||||||
Pb | Th | U | 207Pb/206Pb | σ | 207Pb/235U | σ | 206Pb/238U | σ | 207Pb/235U | σ | 206Pb/238U | σ | 208Pb/232Th | σ | ||||||||||
ZK 31901 二长花 岗岩 (LW01), (92.92± 0.69) Ma, MSWD =2.7 | LW01-01 | 292 | 10 504 | 7 508 | 1.40 | 0.047 83 | 0.000 98 | 0.096 74 | 0.002 24 | 0.014 63 | 0.000 19 | 93.76 | 2.1 | 93.64 | 1.2 | 81.84 | 1.4 | 99 | ||||||
LW01-02 | 131 | 2 010 | 6 834 | 0.29 | 0.049 62 | 0.000 99 | 0.100 55 | 0.002 37 | 0.014 62 | 0.000 17 | 97.28 | 2.2 | 93.58 | 1.1 | 105.74 | 2.4 | 96 | |||||||
LW01-03 | 305 | 9 782 | 6 036 | 1.62 | 0.049 93 | 0.000 98 | 0.097 72 | 0.002 02 | 0.014 18 | 0.000 15 | 94.67 | 1.9 | 90.76 | 1.0 | 93.37 | 1.3 | 95 | |||||||
LW01-04 | 236 | 5 937 | 9 621 | 0.62 | 0.048 49 | 0.000 85 | 0.095 43 | 0.001 78 | 0.014 27 | 0.000 16 | 92.55 | 1.6 | 91.33 | 1.0 | 95.40 | 1.6 | 98 | |||||||
LW01-05 | 401 | 14 012 | 6 960 | 2.01 | 0.050 66 | 0.001 10 | 0.101 00 | 0.002 20 | 0.014 47 | 0.000 17 | 97.70 | 2.0 | 92.62 | 1.1 | 85.50 | 1.3 | 94 | |||||||
LW01-06 | 127 | 2 141 | 7 181 | 0.30 | 0.050 53 | 0.000 96 | 0.098 79 | 0.001 93 | 0.014 15 | 0.000 17 | 95.66 | 1.8 | 90.59 | 1.1 | 93.26 | 2.1 | 94 | |||||||
LW01-07 | 128 | 1 297 | 12 055 | 0.11 | 0.048 32 | 0.000 81 | 0.094 51 | 0.001 78 | 0.014 18 | 0.000 19 | 91.70 | 1.7 | 90.76 | 1.2 | 119.03 | 2.4 | 98 | |||||||
LW01-08 | 246 | 8 028 | 11 582 | 0.69 | 0.046 78 | 0.000 78 | 0.090 76 | 0.001 75 | 0.014 09 | 0.000 22 | 88.21 | 1.6 | 90.22 | 1.4 | 70.63 | 1.0 | 97 | |||||||
LW01-09 | 161 | 2 818 | 12 752 | 0.22 | 0.046 93 | 0.000 74 | 0.097 74 | 0.001 69 | 0.015 07 | 0.000 19 | 94.68 | 1.6 | 96.42 | 1.2 | 85.07 | 1.5 | 98 | |||||||
LW01-10 | 266 | 8 150 | 9 981 | 0.82 | 0.048 76 | 0.000 95 | 0.094 88 | 0.001 92 | 0.014 06 | 0.000 17 | 92.04 | 1.8 | 90.01 | 1.1 | 85.27 | 1.5 | 97 | |||||||
LW01-11 | 233 | 5 134 | 15 311 | 0.34 | 0.048 82 | 0.000 76 | 0.099 46 | 0.001 54 | 0.014 75 | 0.000 17 | 96.28 | 1.4 | 94.40 | 1.1 | 87.42 | 1.8 | 98 | |||||||
LW01-12 | 169 | 401 | 17 590 | 0.02 | 0.050 91 | 0.000 77 | 0.105 68 | 0.001 94 | 0.014 96 | 0.000 17 | 102.01 | 1.8 | 95.72 | 1.1 | 329.72 | 16.2 | 93 | |||||||
LW01-13 | 264 | 5 157 | 21 641 | 0.24 | 0.047 67 | 0.000 76 | 0.096 83 | 0.001 80 | 0.014 68 | 0.000 20 | 93.85 | 1.7 | 93.95 | 1.3 | 79.10 | 1.3 | 99 | |||||||
LW01-14 | 161 | 5 004 | 4 330 | 1.16 | 0.048 61 | 0.001 12 | 0.100 05 | 0.002 38 | 0.014 88 | 0.000 17 | 96.82 | 2.2 | 95.24 | 1.1 | 90.10 | 1.5 | 98 | |||||||
LW01-15 | 102 | 1 802 | 7 882 | 0.23 | 0.047 96 | 0.001 35 | 0.095 54 | 0.002 91 | 0.014 46 | 0.000 18 | 92.66 | 2.7 | 92.58 | 1.1 | 86.78 | 1.9 | 99 | |||||||
LW01-16 | 168 | 3 512 | 10 239 | 0.34 | 0.048 99 | 0.000 80 | 0.097 92 | 0.001 73 | 0.014 49 | 0.000 16 | 94.85 | 1.6 | 92.74 | 1.0 | 90.16 | 1.5 | 97 | |||||||
LW01-17 | 206 | 2 869 | 18 444 | 0.16 | 0.046 49 | 0.000 72 | 0.095 10 | 0.001 61 | 0.014 80 | 0.000 15 | 92.24 | 1.5 | 94.74 | 1.0 | 88.74 | 1.6 | 97 | |||||||
LW01-18 | 149 | 3 740 | 12 842 | 0.29 | 0.049 40 | 0.000 86 | 0.099 41 | 0.002 15 | 0.014 54 | 0.000 21 | 96.23 | 2.0 | 93.06 | 1.3 | 60.11 | 1.6 | 96 | |||||||
LW01-19 | 264 | 3 970 | 23 067 | 0.17 | 0.046 43 | 0.000 68 | 0.091 91 | 0.001 64 | 0.014 32 | 0.000 21 | 89.28 | 1.5 | 91.66 | 1.3 | 96.00 | 1.6 | 97 | |||||||
LW01-20 | 449 | 14 059 | 15 165 | 0.93 | 0.048 28 | 0.000 73 | 0.098 02 | 0.001 82 | 0.014 68 | 0.000 21 | 94.94 | 1.7 | 93.95 | 1.3 | 114.54 | 4.9 | 98 | |||||||
LW01-21 | 649 | 22 961 | 15 164 | 1.51 | 0.047 24 | 0.000 72 | 0.092 46 | 0.001 73 | 0.014 12 | 0.000 18 | 89.80 | 1.6 | 90.40 | 1.2 | 81.84 | 1.3 | 99 | |||||||
LW01-22 | 106 | 3 506 | 2 414 | 1.45 | 0.046 63 | 0.001 46 | 0.091 88 | 0.002 91 | 0.014 36 | 0.000 22 | 89.25 | 2.7 | 91.89 | 1.4 | 87.88 | 1.5 | 97 | |||||||
LW01-23 | 211 | 2 460 | 16 085 | 0.15 | 0.050 53 | 0.000 82 | 0.103 08 | 0.002 45 | 0.014 63 | 0.000 21 | 99.61 | 2.3 | 93.65 | 1.3 | 115.01 | 3.5 | 93 | |||||||
LW01-24 | 648 | 23 183 | 12 706 | 1.82 | 0.047 62 | 0.000 88 | 0.092 13 | 0.002 00 | 0.014 08 | 0.000 24 | 89.49 | 1.9 | 90.15 | 1.5 | 85.98 | 1.4 | 99 | |||||||
岩石 | 点号 | 含量/10-6 | Th/U | 同位素比值 | 年龄/Ma | 谐和度 /% | ||||||||||||||||||
Pb | Th | U | 207Pb/206Pb | σ | 207Pb/235U | σ | 206Pb/238U | σ | 207Pb/235U | σ | 206Pb/238U | σ | 208Pb/232Th | σ | ||||||||||
ZK 31901 二长花 岗岩 (LW01), (92.92± 0.69) Ma, MSWD =2.7 | LW01-25 | 148 | 1 517 | 15 314 | 0.10 | 0.047 41 | 0.000 81 | 0.095 65 | 0.001 76 | 0.014 66 | 0.000 20 | 92.75 | 1.6 | 93.80 | 1.3 | 95.46 | 1.9 | 98 | ||||||
LW01-26 | 257 | 9 135 | 6 740 | 1.36 | 0.049 66 | 0.001 03 | 0.098 21 | 0.002 59 | 0.014 36 | 0.000 29 | 95.12 | 2.4 | 91.88 | 1.8 | 82.45 | 1.7 | 96 | |||||||
LW01-27 | 149 | 4 993 | 3 294 | 1.52 | 0.049 72 | 0.001 59 | 0.101 74 | 0.003 82 | 0.014 83 | 0.000 26 | 98.38 | 3.5 | 94.91 | 1.6 | 91.11 | 1.7 | 96 | |||||||
LW01-28 | 140 | 4 234 | 3 604 | 1.17 | 0.051 66 | 0.001 37 | 0.103 74 | 0.002 76 | 0.014 54 | 0.000 17 | 100.23 | 2.5 | 93.08 | 1.1 | 92.89 | 1.5 | 92 | |||||||
LW01-29 | 214 | 6 161 | 7 448 | 0.83 | 0.052 13 | 0.001 06 | 0.103 10 | 0.002 18 | 0.014 31 | 0.000 15 | 99.63 | 2.0 | 91.57 | 1.0 | 89.58 | 1.4 | 91 | |||||||
LW01-30 | 99 | 1 168 | 9 678 | 0.12 | 0.046 36 | 0.000 85 | 0.096 65 | 0.002 01 | 0.015 05 | 0.000 18 | 93.68 | 1.9 | 96.31 | 1.1 | 93.90 | 2.1 | 97 | |||||||
LW01-31 | 144 | 1 559 | 13 970 | 0.11 | 0.050 04 | 0.001 33 | 0.100 07 | 0.002 96 | 0.014 41 | 0.000 17 | 96.84 | 2.7 | 92.23 | 1.1 | 122.60 | 4.1 | 95 | |||||||
LW01-32 | 288 | 9 163 | 7 044 | 1.30 | 0.049 45 | 0.001 08 | 0.102 77 | 0.002 50 | 0.015 00 | 0.000 20 | 99.33 | 2.3 | 95.97 | 1.3 | 92.42 | 1.4 | 96 | |||||||
岩石 | 点号 | 含量/10-6 | Th/U | 同位素比值 | 年龄/Ma | 谐和度 /% | ||||||||||||||||||
Pb | Th | U | 207Pb/206Pb | σ | 207Pb/235U | σ | 206Pb/238U | σ | 207Pb/235U | σ | 206Pb/238U | σ | 208Pb/232Th | σ | ||||||||||
ZK 40004 黑云 母花 岗岩 (LW15), (92.50± 1.1) Ma, MSWD =2.6 | LW15-03 | 135 | 966 | 15 261 | 0.06 | 0.048 31 | 0.000 65 | 0.097 37 | 0.001 60 | 0.014 56 | 0.000 17 | 94.34 | 1.5 | 93.20 | 1.1 | 107.70 | 2.0 | 98 | ||||||
LW15-04 | 105 | 2 066 | 7 002 | 0.30 | 0.049 47 | 0.000 80 | 0.101 48 | 0.002 09 | 0.014 85 | 0.000 23 | 98.14 | 1.9 | 95.04 | 1.5 | 94.90 | 1.8 | 96 | |||||||
LW15-07 | 48 | 1 211 | 1 870 | 0.65 | 0.053 00 | 0.001 57 | 0.102 79 | 0.003 11 | 0.014 11 | 0.000 21 | 99.35 | 2.9 | 90.30 | 1.3 | 96.30 | 2.0 | 90 | |||||||
LW15-08 | 103 | 1 088 | 9 549 | 0.11 | 0.050 20 | 0.000 91 | 0.100 93 | 0.002 10 | 0.014 56 | 0.000 21 | 97.63 | 1.9 | 93.19 | 1.3 | 121.41 | 4.1 | 95 | |||||||
LW15-10 | 711 | 25 291 | 11 568 | 2.19 | 0.051 62 | 0.000 93 | 0.100 58 | 0.001 82 | 0.014 12 | 0.000 16 | 97.31 | 1.7 | 90.37 | 1.0 | 88.35 | 1.5 | 92 | |||||||
LW15-11 | 92 | 2 742 | 2 114 | 1.30 | 0.048 96 | 0.001 41 | 0.100 55 | 0.003 60 | 0.014 75 | 0.000 27 | 97.28 | 3.3 | 94.38 | 1.7 | 94.87 | 1.6 | 96 | |||||||
LW15-12 | 276 | 8 617 | 5 360 | 1.61 | 0.051 11 | 0.001 06 | 0.100 02 | 0.002 27 | 0.014 14 | 0.000 18 | 96.79 | 2.1 | 90.53 | 1.1 | 92.64 | 1.5 | 93 | |||||||
LW15-13 | 141 | 1 018 | 15 955 | 0.06 | 0.048 24 | 0.000 75 | 0.095 28 | 0.001 51 | 0.014 29 | 0.000 14 | 92.41 | 1.4 | 91.49 | 0.9 | 102.90 | 2.5 | 99 | |||||||
LW15-15 | 551 | 18 309 | 10 052 | 1.82 | 0.048 68 | 0.001 00 | 0.095 54 | 0.002 55 | 0.014 14 | 0.000 23 | 92.65 | 2.4 | 90.52 | 1.5 | 91.84 | 1.8 | 97 | |||||||
LW15-16 | 121 | 1 130 | 12 011 | 0.09 | 0.048 57 | 0.000 82 | 0.098 16 | 0.001 90 | 0.014 59 | 0.000 18 | 95.08 | 1.8 | 93.40 | 1.1 | 103.28 | 2.5 | 98 | |||||||
LW15-18 | 187 | 2 055 | 18 270 | 0.11 | 0.046 78 | 0.000 72 | 0.094 72 | 0.001 58 | 0.014 62 | 0.000 15 | 91.89 | 1.5 | 93.58 | 0.9 | 91.93 | 1.7 | 98 | |||||||
LW15-21 | 386 | 12 341 | 9 754 | 1.27 | 0.047 16 | 0.000 69 | 0.095 22 | 0.001 54 | 0.014 62 | 0.000 17 | 92.36 | 1.4 | 93.55 | 1.1 | 88.46 | 1.3 | 98 | |||||||
LW15-06 | 164 | 4 451 | 6 372 | 0.70 | 0.050 80 | 0.000 99 | 0.107 79 | 0.002 80 | 0.015 30 | 0.000 28 | 103.94 | 2.6 | 97.90 | 1.8 | 91.39 | 1.5 | 94 |
表2 西大明山矿集区燕山期岩浆岩锆石LA-ICP-MS U-Pb年龄定年结果
Table 2 LA-ICP-MS zircon U-Pb data of the Yanshanian magma in the Xidamingshan cluster
岩石 | 点号 | 含量/10-6 | Th/U | 同位素比值 | 年龄/Ma | 谐和度 /% | ||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Pb | Th | U | 207Pb/206Pb | σ | 207Pb/235U | σ | 206Pb/238U | σ | 207Pb/235U | σ | 206Pb/238U | σ | 208Pb/232Th | σ | ||||||||||
那宁 石英 斑岩 (NN02), (93.11± 0.64) Ma, MSWD =1.04 | NN02-04 | 262 | 3 018 | 26 253 | 0.11 | 0.048 35 | 0.000 70 | 0.098 30 | 0.001 72 | 0.014 76 | 0.000 23 | 95.21 | 1.6 | 94.46 | 1.4 | 85.24 | 1.6 | 99 | ||||||
NN02-06 | 174 | 3 710 | 11 378 | 0.33 | 0.047 89 | 0.000 74 | 0.095 51 | 0.001 57 | 0.014 43 | 0.000 15 | 92.63 | 1.5 | 92.36 | 1.0 | 90.09 | 1.6 | 99 | |||||||
NN02-10 | 229 | 4 216 | 16 162 | 0.26 | 0.049 07 | 0.000 85 | 0.098 83 | 0.002 22 | 0.014 60 | 0.000 22 | 95.70 | 2.1 | 93.42 | 1.4 | 96.02 | 1.5 | 97 | |||||||
NN02-11 | 183 | 2 570 | 16 400 | 0.16 | 0.047 06 | 0.000 83 | 0.093 49 | 0.001 59 | 0.014 43 | 0.000 14 | 90.75 | 1.5 | 92.34 | 0.9 | 98.57 | 2.2 | 98 | |||||||
NN02-19 | 159 | 1 942 | 14 314 | 0.14 | 0.048 16 | 0.000 85 | 0.097 77 | 0.001 90 | 0.014 71 | 0.000 16 | 94.72 | 1.8 | 94.14 | 1.0 | 98.93 | 2.0 | 99 | |||||||
NN02-21 | 128 | 2 541 | 8 659 | 0.29 | 0.046 33 | 0.000 94 | 0.094 65 | 0.001 77 | 0.014 71 | 0.000 18 | 91.82 | 1.6 | 94.12 | 1.2 | 91.49 | 1.5 | 97 | |||||||
NN02-23 | 170 | 3 909 | 10 604 | 0.37 | 0.049 08 | 0.000 81 | 0.099 97 | 0.001 70 | 0.014 77 | 0.000 15 | 96.75 | 1.6 | 94.52 | 1.0 | 86.66 | 1.5 | 97 | |||||||
NN02-26 | 416 | 10 862 | 21 164 | 0.51 | 0.047 76 | 0.000 82 | 0.096 05 | 0.001 76 | 0.014 53 | 0.000 14 | 93.12 | 1.6 | 92.97 | 0.9 | 83.24 | 1.4 | 99 | |||||||
NN02-20 | 304 | 2 602 | 27 852 | 0.09 | 0.052 11 | 0.000 85 | 0.104 61 | 0.001 99 | 0.014 52 | 0.000 15 | 101.02 | 1.8 | 92.91 | 1.0 | 142.13 | 6.2 | 91 | |||||||
NN02-14 | 65 | 1 450 | 3 247 | 0.45 | 0.049 64 | 0.001 34 | 0.097 43 | 0.002 65 | 0.014 28 | 0.000 15 | 94.40 | 2.5 | 91.38 | 1.0 | 94.57 | 1.9 | 96 | |||||||
岩石 | 点号 | 含量/10-6 | Th/U | 同位素比值 | 年龄/Ma | 谐和度 /% | ||||||||||||||||||
Pb | Th | U | 207Pb/206Pb | σ | 207Pb/235U | σ | 206Pb/238U | σ | 207Pb/235U | σ | 206Pb/238U | σ | 208Pb/232Th | σ | ||||||||||
ZK 31901 二长花 岗岩 (LW01), (92.92± 0.69) Ma, MSWD =2.7 | LW01-01 | 292 | 10 504 | 7 508 | 1.40 | 0.047 83 | 0.000 98 | 0.096 74 | 0.002 24 | 0.014 63 | 0.000 19 | 93.76 | 2.1 | 93.64 | 1.2 | 81.84 | 1.4 | 99 | ||||||
LW01-02 | 131 | 2 010 | 6 834 | 0.29 | 0.049 62 | 0.000 99 | 0.100 55 | 0.002 37 | 0.014 62 | 0.000 17 | 97.28 | 2.2 | 93.58 | 1.1 | 105.74 | 2.4 | 96 | |||||||
LW01-03 | 305 | 9 782 | 6 036 | 1.62 | 0.049 93 | 0.000 98 | 0.097 72 | 0.002 02 | 0.014 18 | 0.000 15 | 94.67 | 1.9 | 90.76 | 1.0 | 93.37 | 1.3 | 95 | |||||||
LW01-04 | 236 | 5 937 | 9 621 | 0.62 | 0.048 49 | 0.000 85 | 0.095 43 | 0.001 78 | 0.014 27 | 0.000 16 | 92.55 | 1.6 | 91.33 | 1.0 | 95.40 | 1.6 | 98 | |||||||
LW01-05 | 401 | 14 012 | 6 960 | 2.01 | 0.050 66 | 0.001 10 | 0.101 00 | 0.002 20 | 0.014 47 | 0.000 17 | 97.70 | 2.0 | 92.62 | 1.1 | 85.50 | 1.3 | 94 | |||||||
LW01-06 | 127 | 2 141 | 7 181 | 0.30 | 0.050 53 | 0.000 96 | 0.098 79 | 0.001 93 | 0.014 15 | 0.000 17 | 95.66 | 1.8 | 90.59 | 1.1 | 93.26 | 2.1 | 94 | |||||||
LW01-07 | 128 | 1 297 | 12 055 | 0.11 | 0.048 32 | 0.000 81 | 0.094 51 | 0.001 78 | 0.014 18 | 0.000 19 | 91.70 | 1.7 | 90.76 | 1.2 | 119.03 | 2.4 | 98 | |||||||
LW01-08 | 246 | 8 028 | 11 582 | 0.69 | 0.046 78 | 0.000 78 | 0.090 76 | 0.001 75 | 0.014 09 | 0.000 22 | 88.21 | 1.6 | 90.22 | 1.4 | 70.63 | 1.0 | 97 | |||||||
LW01-09 | 161 | 2 818 | 12 752 | 0.22 | 0.046 93 | 0.000 74 | 0.097 74 | 0.001 69 | 0.015 07 | 0.000 19 | 94.68 | 1.6 | 96.42 | 1.2 | 85.07 | 1.5 | 98 | |||||||
LW01-10 | 266 | 8 150 | 9 981 | 0.82 | 0.048 76 | 0.000 95 | 0.094 88 | 0.001 92 | 0.014 06 | 0.000 17 | 92.04 | 1.8 | 90.01 | 1.1 | 85.27 | 1.5 | 97 | |||||||
LW01-11 | 233 | 5 134 | 15 311 | 0.34 | 0.048 82 | 0.000 76 | 0.099 46 | 0.001 54 | 0.014 75 | 0.000 17 | 96.28 | 1.4 | 94.40 | 1.1 | 87.42 | 1.8 | 98 | |||||||
LW01-12 | 169 | 401 | 17 590 | 0.02 | 0.050 91 | 0.000 77 | 0.105 68 | 0.001 94 | 0.014 96 | 0.000 17 | 102.01 | 1.8 | 95.72 | 1.1 | 329.72 | 16.2 | 93 | |||||||
LW01-13 | 264 | 5 157 | 21 641 | 0.24 | 0.047 67 | 0.000 76 | 0.096 83 | 0.001 80 | 0.014 68 | 0.000 20 | 93.85 | 1.7 | 93.95 | 1.3 | 79.10 | 1.3 | 99 | |||||||
LW01-14 | 161 | 5 004 | 4 330 | 1.16 | 0.048 61 | 0.001 12 | 0.100 05 | 0.002 38 | 0.014 88 | 0.000 17 | 96.82 | 2.2 | 95.24 | 1.1 | 90.10 | 1.5 | 98 | |||||||
LW01-15 | 102 | 1 802 | 7 882 | 0.23 | 0.047 96 | 0.001 35 | 0.095 54 | 0.002 91 | 0.014 46 | 0.000 18 | 92.66 | 2.7 | 92.58 | 1.1 | 86.78 | 1.9 | 99 | |||||||
LW01-16 | 168 | 3 512 | 10 239 | 0.34 | 0.048 99 | 0.000 80 | 0.097 92 | 0.001 73 | 0.014 49 | 0.000 16 | 94.85 | 1.6 | 92.74 | 1.0 | 90.16 | 1.5 | 97 | |||||||
LW01-17 | 206 | 2 869 | 18 444 | 0.16 | 0.046 49 | 0.000 72 | 0.095 10 | 0.001 61 | 0.014 80 | 0.000 15 | 92.24 | 1.5 | 94.74 | 1.0 | 88.74 | 1.6 | 97 | |||||||
LW01-18 | 149 | 3 740 | 12 842 | 0.29 | 0.049 40 | 0.000 86 | 0.099 41 | 0.002 15 | 0.014 54 | 0.000 21 | 96.23 | 2.0 | 93.06 | 1.3 | 60.11 | 1.6 | 96 | |||||||
LW01-19 | 264 | 3 970 | 23 067 | 0.17 | 0.046 43 | 0.000 68 | 0.091 91 | 0.001 64 | 0.014 32 | 0.000 21 | 89.28 | 1.5 | 91.66 | 1.3 | 96.00 | 1.6 | 97 | |||||||
LW01-20 | 449 | 14 059 | 15 165 | 0.93 | 0.048 28 | 0.000 73 | 0.098 02 | 0.001 82 | 0.014 68 | 0.000 21 | 94.94 | 1.7 | 93.95 | 1.3 | 114.54 | 4.9 | 98 | |||||||
LW01-21 | 649 | 22 961 | 15 164 | 1.51 | 0.047 24 | 0.000 72 | 0.092 46 | 0.001 73 | 0.014 12 | 0.000 18 | 89.80 | 1.6 | 90.40 | 1.2 | 81.84 | 1.3 | 99 | |||||||
LW01-22 | 106 | 3 506 | 2 414 | 1.45 | 0.046 63 | 0.001 46 | 0.091 88 | 0.002 91 | 0.014 36 | 0.000 22 | 89.25 | 2.7 | 91.89 | 1.4 | 87.88 | 1.5 | 97 | |||||||
LW01-23 | 211 | 2 460 | 16 085 | 0.15 | 0.050 53 | 0.000 82 | 0.103 08 | 0.002 45 | 0.014 63 | 0.000 21 | 99.61 | 2.3 | 93.65 | 1.3 | 115.01 | 3.5 | 93 | |||||||
LW01-24 | 648 | 23 183 | 12 706 | 1.82 | 0.047 62 | 0.000 88 | 0.092 13 | 0.002 00 | 0.014 08 | 0.000 24 | 89.49 | 1.9 | 90.15 | 1.5 | 85.98 | 1.4 | 99 | |||||||
岩石 | 点号 | 含量/10-6 | Th/U | 同位素比值 | 年龄/Ma | 谐和度 /% | ||||||||||||||||||
Pb | Th | U | 207Pb/206Pb | σ | 207Pb/235U | σ | 206Pb/238U | σ | 207Pb/235U | σ | 206Pb/238U | σ | 208Pb/232Th | σ | ||||||||||
ZK 31901 二长花 岗岩 (LW01), (92.92± 0.69) Ma, MSWD =2.7 | LW01-25 | 148 | 1 517 | 15 314 | 0.10 | 0.047 41 | 0.000 81 | 0.095 65 | 0.001 76 | 0.014 66 | 0.000 20 | 92.75 | 1.6 | 93.80 | 1.3 | 95.46 | 1.9 | 98 | ||||||
LW01-26 | 257 | 9 135 | 6 740 | 1.36 | 0.049 66 | 0.001 03 | 0.098 21 | 0.002 59 | 0.014 36 | 0.000 29 | 95.12 | 2.4 | 91.88 | 1.8 | 82.45 | 1.7 | 96 | |||||||
LW01-27 | 149 | 4 993 | 3 294 | 1.52 | 0.049 72 | 0.001 59 | 0.101 74 | 0.003 82 | 0.014 83 | 0.000 26 | 98.38 | 3.5 | 94.91 | 1.6 | 91.11 | 1.7 | 96 | |||||||
LW01-28 | 140 | 4 234 | 3 604 | 1.17 | 0.051 66 | 0.001 37 | 0.103 74 | 0.002 76 | 0.014 54 | 0.000 17 | 100.23 | 2.5 | 93.08 | 1.1 | 92.89 | 1.5 | 92 | |||||||
LW01-29 | 214 | 6 161 | 7 448 | 0.83 | 0.052 13 | 0.001 06 | 0.103 10 | 0.002 18 | 0.014 31 | 0.000 15 | 99.63 | 2.0 | 91.57 | 1.0 | 89.58 | 1.4 | 91 | |||||||
LW01-30 | 99 | 1 168 | 9 678 | 0.12 | 0.046 36 | 0.000 85 | 0.096 65 | 0.002 01 | 0.015 05 | 0.000 18 | 93.68 | 1.9 | 96.31 | 1.1 | 93.90 | 2.1 | 97 | |||||||
LW01-31 | 144 | 1 559 | 13 970 | 0.11 | 0.050 04 | 0.001 33 | 0.100 07 | 0.002 96 | 0.014 41 | 0.000 17 | 96.84 | 2.7 | 92.23 | 1.1 | 122.60 | 4.1 | 95 | |||||||
LW01-32 | 288 | 9 163 | 7 044 | 1.30 | 0.049 45 | 0.001 08 | 0.102 77 | 0.002 50 | 0.015 00 | 0.000 20 | 99.33 | 2.3 | 95.97 | 1.3 | 92.42 | 1.4 | 96 | |||||||
岩石 | 点号 | 含量/10-6 | Th/U | 同位素比值 | 年龄/Ma | 谐和度 /% | ||||||||||||||||||
Pb | Th | U | 207Pb/206Pb | σ | 207Pb/235U | σ | 206Pb/238U | σ | 207Pb/235U | σ | 206Pb/238U | σ | 208Pb/232Th | σ | ||||||||||
ZK 40004 黑云 母花 岗岩 (LW15), (92.50± 1.1) Ma, MSWD =2.6 | LW15-03 | 135 | 966 | 15 261 | 0.06 | 0.048 31 | 0.000 65 | 0.097 37 | 0.001 60 | 0.014 56 | 0.000 17 | 94.34 | 1.5 | 93.20 | 1.1 | 107.70 | 2.0 | 98 | ||||||
LW15-04 | 105 | 2 066 | 7 002 | 0.30 | 0.049 47 | 0.000 80 | 0.101 48 | 0.002 09 | 0.014 85 | 0.000 23 | 98.14 | 1.9 | 95.04 | 1.5 | 94.90 | 1.8 | 96 | |||||||
LW15-07 | 48 | 1 211 | 1 870 | 0.65 | 0.053 00 | 0.001 57 | 0.102 79 | 0.003 11 | 0.014 11 | 0.000 21 | 99.35 | 2.9 | 90.30 | 1.3 | 96.30 | 2.0 | 90 | |||||||
LW15-08 | 103 | 1 088 | 9 549 | 0.11 | 0.050 20 | 0.000 91 | 0.100 93 | 0.002 10 | 0.014 56 | 0.000 21 | 97.63 | 1.9 | 93.19 | 1.3 | 121.41 | 4.1 | 95 | |||||||
LW15-10 | 711 | 25 291 | 11 568 | 2.19 | 0.051 62 | 0.000 93 | 0.100 58 | 0.001 82 | 0.014 12 | 0.000 16 | 97.31 | 1.7 | 90.37 | 1.0 | 88.35 | 1.5 | 92 | |||||||
LW15-11 | 92 | 2 742 | 2 114 | 1.30 | 0.048 96 | 0.001 41 | 0.100 55 | 0.003 60 | 0.014 75 | 0.000 27 | 97.28 | 3.3 | 94.38 | 1.7 | 94.87 | 1.6 | 96 | |||||||
LW15-12 | 276 | 8 617 | 5 360 | 1.61 | 0.051 11 | 0.001 06 | 0.100 02 | 0.002 27 | 0.014 14 | 0.000 18 | 96.79 | 2.1 | 90.53 | 1.1 | 92.64 | 1.5 | 93 | |||||||
LW15-13 | 141 | 1 018 | 15 955 | 0.06 | 0.048 24 | 0.000 75 | 0.095 28 | 0.001 51 | 0.014 29 | 0.000 14 | 92.41 | 1.4 | 91.49 | 0.9 | 102.90 | 2.5 | 99 | |||||||
LW15-15 | 551 | 18 309 | 10 052 | 1.82 | 0.048 68 | 0.001 00 | 0.095 54 | 0.002 55 | 0.014 14 | 0.000 23 | 92.65 | 2.4 | 90.52 | 1.5 | 91.84 | 1.8 | 97 | |||||||
LW15-16 | 121 | 1 130 | 12 011 | 0.09 | 0.048 57 | 0.000 82 | 0.098 16 | 0.001 90 | 0.014 59 | 0.000 18 | 95.08 | 1.8 | 93.40 | 1.1 | 103.28 | 2.5 | 98 | |||||||
LW15-18 | 187 | 2 055 | 18 270 | 0.11 | 0.046 78 | 0.000 72 | 0.094 72 | 0.001 58 | 0.014 62 | 0.000 15 | 91.89 | 1.5 | 93.58 | 0.9 | 91.93 | 1.7 | 98 | |||||||
LW15-21 | 386 | 12 341 | 9 754 | 1.27 | 0.047 16 | 0.000 69 | 0.095 22 | 0.001 54 | 0.014 62 | 0.000 17 | 92.36 | 1.4 | 93.55 | 1.1 | 88.46 | 1.3 | 98 | |||||||
LW15-06 | 164 | 4 451 | 6 372 | 0.70 | 0.050 80 | 0.000 99 | 0.107 79 | 0.002 80 | 0.015 30 | 0.000 28 | 103.94 | 2.6 | 97.90 | 1.8 | 91.39 | 1.5 | 94 |
测点 | 176Yb/177Hf | 176Lu/177Hf | 176Hf/177Hf | 2σ | 年龄/Ma | εHf(0) | εHf(t) | TDM1 | TDM2 | fLu/Hf | |
---|---|---|---|---|---|---|---|---|---|---|---|
那宁 石英 斑岩 (NN02) | NN02-04 | 0.017 553 | 0.000 655 | 0.282 194 | 0.000 023 | 94.46 | -20.4 | -18.4 | 1 478 | 2 326 | -0.980 274 |
NN02-06 | 0.027 249 | 0.000 977 | 0.282 533 | 0.000 021 | 92.36 | -8.4 | -6.5 | 1 016 | 1 569 | -0.970 580 | |
NN02-11 | 0.045 272 | 0.001 566 | 0.282 683 | 0.000 022 | 92.34 | -3.2 | -1.2 | 819 | 1 236 | -0.952 839 | |
NN02-19 | 0.032 451 | 0.001 146 | 0.282 537 | 0.000 023 | 94.14 | -8.3 | -6.3 | 1 015 | 1 562 | -0.965 490 | |
NN02-21 | 0.021 194 | 0.000 776 | 0.282 497 | 0.000 020 | 94.12 | -9.7 | -7.7 | 1 062 | 1 650 | -0.976 640 | |
NN02-23 | 0.041 380 | 0.001 451 | 0.282 526 | 0.000 023 | 94.52 | -8.7 | -6.7 | 1 039 | 1 586 | -0.956 287 | |
NN02-26 | 0.052 688 | 0.001 931 | 0.282 532 | 0.000 022 | 92.97 | -8.5 | -6.6 | 1 045 | 1 576 | -0.941 840 | |
NN02-14 | 0.055 506 | 0.002 104 | 0.282 623 | 0.000 022 | 91.38 | -5.3 | -3.4 | 917 | 1 371 | -0.936 623 | |
ZK 31901 二长花 岗岩 (LW01) | LW01-01 | 0.057 400 | 0.001 964 | 0.282 553 | 0.000 039 | 93.64 | -7.7 | -5.8 | 1 014 | 1 527 | -0.940 851 |
LW01-02 | 0.047 734 | 0.001 672 | 0.282 545 | 0.000 022 | 93.58 | -8.0 | -6.1 | 1 018 | 1 545 | -0.949 633 | |
LW01-03 | 0.081 764 | 0.002 695 | 0.282 588 | 0.000 026 | 90.76 | -6.5 | -4.7 | 984 | 1 453 | -0.918 823 | |
LW01-04 | 0.073 351 | 0.002 573 | 0.282 592 | 0.000 023 | 91.33 | -6.4 | -4.5 | 975 | 1 445 | -0.922 496 | |
LW01-05 | 0.049 618 | 0.001 702 | 0.282 547 | 0.000 021 | 92.60 | -7.9 | -6.0 | 1 016 | 1 541 | -0.948 750 | |
LW01-06 | 0.063 284 | 0.002 360 | 0.282 564 | 0.000 040 | 90.59 | -7.4 | -5.5 | 1 010 | 1 507 | -0.928 905 | |
LW01-07 | 0.047 789 | 0.001 771 | 0.282 544 | 0.000 019 | 90.76 | -8.1 | -6.2 | 1 023 | 1 550 | -0.946 655 | |
LW01-08 | 0.056 025 | 0.001 946 | 0.282 561 | 0.000 021 | 90.22 | -7.5 | -5.6 | 1 003 | 1 513 | -0.941 394 | |
LW01-09 | 0.055 295 | 0.001 986 | 0.282 497 | 0.000 021 | 96.42 | -9.7 | -7.7 | 1 096 | 1 651 | -0.940 193 | |
LW01-10 | 0.072 069 | 0.002 575 | 0.282 728 | 0.000 029 | 90.01 | -1.6 | 0.3 | 775 | 1 139 | -0.922 443 | |
LW01-11 | 0.039 070 | 0.001 332 | 0.282 550 | 0.000 022 | 94.40 | -7.9 | -5.9 | 1 002 | 1 533 | -0.959 878 | |
LW01-12 | 0.086 888 | 0.003 032 | 0.282 502 | 0.000 182 | 95.72 | -9.6 | -7.7 | 1 121 | 1 646 | -0.908 678 | |
LW01-13 | 0.050 289 | 0.001 699 | 0.282 594 | 0.000 027 | 93.95 | -6.3 | -4.3 | 949 | 1 435 | -0.948 827 | |
LW01-14 | 0.049 415 | 0.001 784 | 0.282 571 | 0.000 023 | 92.23 | -7.1 | -5.2 | 984 | 1 488 | -0.946 266 | |
LW01-15 | 0.027 949 | 0.001 091 | 0.282 169 | 0.000 045 | 92.58 | -21.3 | -19.4 | 1 530 | 2 385 | -0.967 127 | |
LW01-16 | 0.037 307 | 0.001 379 | 0.282 641 | 0.000 024 | 92.74 | -4.6 | -2.7 | 875 | 1 330 | -0.958 458 | |
LW01-17 | 0.044 998 | 0.001 650 | 0.282 534 | 0.000 017 | 94.74 | -8.4 | -6.5 | 1 034 | 1 570 | -0.950 293 | |
LW01-18 | 0.052 986 | 0.001 943 | 0.282 517 | 0.000 024 | 93.06 | -9.0 | -7.1 | 1 066 | 1 609 | -0.941 488 | |
LW01-19 | 0.048 802 | 0.001 686 | 0.282 529 | 0.000 027 | 91.66 | -8.6 | -6.7 | 1 041 | 1 582 | -0.949 209 | |
LW01-20 | 0.064 364 | 0.002 309 | 0.282 574 | 0.000 023 | 93.95 | -7.0 | -5.1 | 994 | 1 482 | -0.930 456 | |
LW01-21 | 0.050 132 | 0.001 786 | 0.282 577 | 0.000 024 | 90.40 | -6.9 | -5.0 | 975 | 1 475 | -0.946 196 | |
LW01-22 | 0.042 118 | 0.001 457 | 0.282 570 | 0.000 028 | 91.89 | -7.1 | -5.2 | 976 | 1 488 | -0.956 104 | |
LW01-23 | 0.025 674 | 0.000 917 | 0.282 629 | 0.000 020 | 93.65 | -5.1 | -3.1 | 881 | 1 354 | -0.972 387 | |
LW01-24 | 0.078 144 | 0.002 671 | 0.282 696 | 0.000 024 | 90.15 | -2.7 | -0.9 | 825 | 1 212 | -0.919 538 | |
LW01-25 | 0.037 890 | 0.001 427 | 0.282 556 | 0.000 025 | 93.80 | -7.6 | -5.7 | 996 | 1 519 | -0.957 021 | |
LW01-26 | 0.040 122 | 0.001 410 | 0.282 587 | 0.000 024 | 91.88 | -6.5 | -4.6 | 951 | 1 450 | -0.957 538 | |
LW01-27 | 0.070 580 | 0.002 497 | 0.282 589 | 0.000 037 | 94.91 | -6.5 | -4.5 | 977 | 1 448 | -0.924 787 | |
LW01-28 | 0.051 980 | 0.001 839 | 0.282 590 | 0.000 021 | 91.57 | -6.4 | -4.5 | 958 | 1 445 | -0.944 598 | |
LW01-29 | 0.029 554 | 0.001 066 | 0.282 550 | 0.000 019 | 93.08 | -7.9 | -5.9 | 996 | 1 533 | -0.967 878 | |
LW01-30 | 0.061 614 | 0.002 220 | 0.282 586 | 0.000 021 | 96.31 | -6.6 | -4.6 | 974 | 1 453 | -0.933 126 | |
LW01-31 | 0.061 560 | 0.002 217 | 0.282 575 | 0.000 023 | 95.24 | -7.0 | -5.0 | 989 | 1 478 | -0.933 213 | |
LW01-32 | 0.057 132 | 0.002 085 | 0.282 529 | 0.000 034 | 95.97 | -8.6 | -6.6 | 1 053 | 1 581 | -0.937 191 | |
ZK 40004 黑云母 花岗岩 (LW15) | LW15-21 | 0.076 118 | 0.002 707 | 0.282 617 | 0.000 027 | 93.55 | -5.5 | -3.6 | 941 | 1 386 | -0.918 461 |
LW15-16 | 0.057 945 | 0.002 137 | 0.282 548 | 0.000 023 | 93.40 | -7.9 | -6.0 | 1 026 | 1 539 | -0.935 647 | |
LW15-10 | 0.023 874 | 0.000 844 | 0.282 565 | 0.000 020 | 90.37 | -7.3 | -5.4 | 968 | 1 500 | -0.974 568 | |
LW15-08 | 0.071 919 | 0.002 808 | 0.282 547 | 0.000 035 | 93.19 | -8.0 | -6.1 | 1 047 | 1 545 | -0.915 407 | |
LW15-03 | 0.025 285 | 0.000 906 | 0.282 371 | 0.000 027 | 93.20 | -14.2 | -12.2 | 1 241 | 1 933 | -0.972 710 |
表3 西大明山矿集区燕山期岩浆岩锆石Hf同位素组成
Table 3 Zircon Hf isotope data for the Yanshanian magma in the Xidamingshan cluster
测点 | 176Yb/177Hf | 176Lu/177Hf | 176Hf/177Hf | 2σ | 年龄/Ma | εHf(0) | εHf(t) | TDM1 | TDM2 | fLu/Hf | |
---|---|---|---|---|---|---|---|---|---|---|---|
那宁 石英 斑岩 (NN02) | NN02-04 | 0.017 553 | 0.000 655 | 0.282 194 | 0.000 023 | 94.46 | -20.4 | -18.4 | 1 478 | 2 326 | -0.980 274 |
NN02-06 | 0.027 249 | 0.000 977 | 0.282 533 | 0.000 021 | 92.36 | -8.4 | -6.5 | 1 016 | 1 569 | -0.970 580 | |
NN02-11 | 0.045 272 | 0.001 566 | 0.282 683 | 0.000 022 | 92.34 | -3.2 | -1.2 | 819 | 1 236 | -0.952 839 | |
NN02-19 | 0.032 451 | 0.001 146 | 0.282 537 | 0.000 023 | 94.14 | -8.3 | -6.3 | 1 015 | 1 562 | -0.965 490 | |
NN02-21 | 0.021 194 | 0.000 776 | 0.282 497 | 0.000 020 | 94.12 | -9.7 | -7.7 | 1 062 | 1 650 | -0.976 640 | |
NN02-23 | 0.041 380 | 0.001 451 | 0.282 526 | 0.000 023 | 94.52 | -8.7 | -6.7 | 1 039 | 1 586 | -0.956 287 | |
NN02-26 | 0.052 688 | 0.001 931 | 0.282 532 | 0.000 022 | 92.97 | -8.5 | -6.6 | 1 045 | 1 576 | -0.941 840 | |
NN02-14 | 0.055 506 | 0.002 104 | 0.282 623 | 0.000 022 | 91.38 | -5.3 | -3.4 | 917 | 1 371 | -0.936 623 | |
ZK 31901 二长花 岗岩 (LW01) | LW01-01 | 0.057 400 | 0.001 964 | 0.282 553 | 0.000 039 | 93.64 | -7.7 | -5.8 | 1 014 | 1 527 | -0.940 851 |
LW01-02 | 0.047 734 | 0.001 672 | 0.282 545 | 0.000 022 | 93.58 | -8.0 | -6.1 | 1 018 | 1 545 | -0.949 633 | |
LW01-03 | 0.081 764 | 0.002 695 | 0.282 588 | 0.000 026 | 90.76 | -6.5 | -4.7 | 984 | 1 453 | -0.918 823 | |
LW01-04 | 0.073 351 | 0.002 573 | 0.282 592 | 0.000 023 | 91.33 | -6.4 | -4.5 | 975 | 1 445 | -0.922 496 | |
LW01-05 | 0.049 618 | 0.001 702 | 0.282 547 | 0.000 021 | 92.60 | -7.9 | -6.0 | 1 016 | 1 541 | -0.948 750 | |
LW01-06 | 0.063 284 | 0.002 360 | 0.282 564 | 0.000 040 | 90.59 | -7.4 | -5.5 | 1 010 | 1 507 | -0.928 905 | |
LW01-07 | 0.047 789 | 0.001 771 | 0.282 544 | 0.000 019 | 90.76 | -8.1 | -6.2 | 1 023 | 1 550 | -0.946 655 | |
LW01-08 | 0.056 025 | 0.001 946 | 0.282 561 | 0.000 021 | 90.22 | -7.5 | -5.6 | 1 003 | 1 513 | -0.941 394 | |
LW01-09 | 0.055 295 | 0.001 986 | 0.282 497 | 0.000 021 | 96.42 | -9.7 | -7.7 | 1 096 | 1 651 | -0.940 193 | |
LW01-10 | 0.072 069 | 0.002 575 | 0.282 728 | 0.000 029 | 90.01 | -1.6 | 0.3 | 775 | 1 139 | -0.922 443 | |
LW01-11 | 0.039 070 | 0.001 332 | 0.282 550 | 0.000 022 | 94.40 | -7.9 | -5.9 | 1 002 | 1 533 | -0.959 878 | |
LW01-12 | 0.086 888 | 0.003 032 | 0.282 502 | 0.000 182 | 95.72 | -9.6 | -7.7 | 1 121 | 1 646 | -0.908 678 | |
LW01-13 | 0.050 289 | 0.001 699 | 0.282 594 | 0.000 027 | 93.95 | -6.3 | -4.3 | 949 | 1 435 | -0.948 827 | |
LW01-14 | 0.049 415 | 0.001 784 | 0.282 571 | 0.000 023 | 92.23 | -7.1 | -5.2 | 984 | 1 488 | -0.946 266 | |
LW01-15 | 0.027 949 | 0.001 091 | 0.282 169 | 0.000 045 | 92.58 | -21.3 | -19.4 | 1 530 | 2 385 | -0.967 127 | |
LW01-16 | 0.037 307 | 0.001 379 | 0.282 641 | 0.000 024 | 92.74 | -4.6 | -2.7 | 875 | 1 330 | -0.958 458 | |
LW01-17 | 0.044 998 | 0.001 650 | 0.282 534 | 0.000 017 | 94.74 | -8.4 | -6.5 | 1 034 | 1 570 | -0.950 293 | |
LW01-18 | 0.052 986 | 0.001 943 | 0.282 517 | 0.000 024 | 93.06 | -9.0 | -7.1 | 1 066 | 1 609 | -0.941 488 | |
LW01-19 | 0.048 802 | 0.001 686 | 0.282 529 | 0.000 027 | 91.66 | -8.6 | -6.7 | 1 041 | 1 582 | -0.949 209 | |
LW01-20 | 0.064 364 | 0.002 309 | 0.282 574 | 0.000 023 | 93.95 | -7.0 | -5.1 | 994 | 1 482 | -0.930 456 | |
LW01-21 | 0.050 132 | 0.001 786 | 0.282 577 | 0.000 024 | 90.40 | -6.9 | -5.0 | 975 | 1 475 | -0.946 196 | |
LW01-22 | 0.042 118 | 0.001 457 | 0.282 570 | 0.000 028 | 91.89 | -7.1 | -5.2 | 976 | 1 488 | -0.956 104 | |
LW01-23 | 0.025 674 | 0.000 917 | 0.282 629 | 0.000 020 | 93.65 | -5.1 | -3.1 | 881 | 1 354 | -0.972 387 | |
LW01-24 | 0.078 144 | 0.002 671 | 0.282 696 | 0.000 024 | 90.15 | -2.7 | -0.9 | 825 | 1 212 | -0.919 538 | |
LW01-25 | 0.037 890 | 0.001 427 | 0.282 556 | 0.000 025 | 93.80 | -7.6 | -5.7 | 996 | 1 519 | -0.957 021 | |
LW01-26 | 0.040 122 | 0.001 410 | 0.282 587 | 0.000 024 | 91.88 | -6.5 | -4.6 | 951 | 1 450 | -0.957 538 | |
LW01-27 | 0.070 580 | 0.002 497 | 0.282 589 | 0.000 037 | 94.91 | -6.5 | -4.5 | 977 | 1 448 | -0.924 787 | |
LW01-28 | 0.051 980 | 0.001 839 | 0.282 590 | 0.000 021 | 91.57 | -6.4 | -4.5 | 958 | 1 445 | -0.944 598 | |
LW01-29 | 0.029 554 | 0.001 066 | 0.282 550 | 0.000 019 | 93.08 | -7.9 | -5.9 | 996 | 1 533 | -0.967 878 | |
LW01-30 | 0.061 614 | 0.002 220 | 0.282 586 | 0.000 021 | 96.31 | -6.6 | -4.6 | 974 | 1 453 | -0.933 126 | |
LW01-31 | 0.061 560 | 0.002 217 | 0.282 575 | 0.000 023 | 95.24 | -7.0 | -5.0 | 989 | 1 478 | -0.933 213 | |
LW01-32 | 0.057 132 | 0.002 085 | 0.282 529 | 0.000 034 | 95.97 | -8.6 | -6.6 | 1 053 | 1 581 | -0.937 191 | |
ZK 40004 黑云母 花岗岩 (LW15) | LW15-21 | 0.076 118 | 0.002 707 | 0.282 617 | 0.000 027 | 93.55 | -5.5 | -3.6 | 941 | 1 386 | -0.918 461 |
LW15-16 | 0.057 945 | 0.002 137 | 0.282 548 | 0.000 023 | 93.40 | -7.9 | -6.0 | 1 026 | 1 539 | -0.935 647 | |
LW15-10 | 0.023 874 | 0.000 844 | 0.282 565 | 0.000 020 | 90.37 | -7.3 | -5.4 | 968 | 1 500 | -0.974 568 | |
LW15-08 | 0.071 919 | 0.002 808 | 0.282 547 | 0.000 035 | 93.19 | -8.0 | -6.1 | 1 047 | 1 545 | -0.915 407 | |
LW15-03 | 0.025 285 | 0.000 906 | 0.282 371 | 0.000 027 | 93.20 | -14.2 | -12.2 | 1 241 | 1 933 | -0.972 710 |
图5 西大明山燕山期岩浆岩及右江褶皱带周缘锆石εHf (t)-U-Pb年龄图解
Fig.5 εHf (t) vs age plots for zircons of the Yanshanian magma in the Xidamingshan cluster and granites in the margin of Youjiang fold belt
[1] | 华仁民, 朱金初, 赵一英, 等. 右江褶皱带有色金属矿床成矿系列初步研究[J]. 高校地质学报, 1997. 3(2):183-191. |
[2] |
DENG J, WANG Q F, LI G J, et al. Cenozoic tectono-magmatic and metallogenic processes in the Sanjiang region,southwestern China[J]. Earth-Science Reviews, 2014, 138:268-299.
DOI URL |
[3] | 陈懋弘, 陆刚, 李新华. 桂西北地区石英斑岩脉白云母 40Ar/39Ar年龄及其地质意义[J]. 高校地质学报, 2012, 18(1):106-116. |
[4] | 胡瑞忠, 毕献武, 彭建堂, 等. 华南地区中生代以来岩石圈伸展及铀矿成矿关系研究的若干问题[J]. 矿床地质, 2010, 26(2):139-152. |
[5] | 毛景文, 陈懋弘, 袁顺达, 等. 华南地区钦杭成矿带地质特征和矿床时空分布规律[J]. 地质学报, 2011, 85(5):636-658. |
[6] | 周永章, 李兴远, 郑义, 等. 钦杭结合带成矿地质背景及成矿规律[J]. 岩石学报, 2017, 33(3):667-681. |
[7] | 付伟, 冯佐海, 李赛赛, 等. 广西西大明山W-Bi-Pb-Zn-Ag多金属矿集区:一个与隐伏岩体相关的岩浆热液成矿系统?[C]// 中国地球物理学会.2014年中国地球科学联合学术年会——专题35:汇聚板块边缘热液矿床成矿机制与勘查应用论文集. 北京: 中国地球物理学会, 2014:1879-1881. |
[8] | 蔡明海, 何龙清, 刘国庆, 等. 广西大厂锡矿田侵入岩SHRIMP锆石U-Pb年龄及其意义[J]. 地质论评, 2006, 52(3):409-414. |
[9] | 蔡明海, 梁婷, 吴德成. 广西大厂锡多金属矿田亢马矿床地质特征及成矿时代[J]. 地质学报, 2005, 79(2):262-268. |
[10] | 蔡明海, 梁婷, 韦利可, 等. 广西大厂锡多金属矿田铜坑—长坡92号矿体Rb-Sr测年及其地质意义[J]. 华南地质与矿产, 2006(2):31-36. |
[11] | 梁婷, 王登红, 侯可军, 等. 广西大厂笼箱盖复式岩体的LA-MC-ICP-MS锆石U-Pb年龄及其地质意义[J]. 岩石学报, 2011, 27(6):1624-1636. |
[12] | 王新宇, 黄宏伟, 陈能松, 等. 广西大厂矿田长坡—铜坑锡多金属矿床锡石LA-MC-ICP-MS U-Pb年龄及其地质意义[J]. 地质论评, 2015, 61(4):892-900. |
[13] | 蔺志永, 王登红, 李水如. 广西王社铜钨矿床地质特征及其成矿时代[J]. 地质学报, 2008, 82(11):1565-1571. |
[14] | 李水如, 王登红, 梁婷, 等. 广西大明山钨矿区成矿时代及其找矿前景分析[J]. 地质学报, 2008, 82(7):873-879. |
[15] | 陈海, 琼慧. 广西凤凰山银矿床成因探讨[J]. 南方国土资源, 1997, 10(2):37-44. |
[16] |
TU W, DU Y S, WANG G W, et al. Cordilleran vein type Pb-Zn-polymetallic deposits of the Xidamingshan district,Guangxi,SW China:Fluid inclusion and geochemical studies[J]. Geology of Ore Deposits, 2013, 55(6):494-502.
DOI URL |
[17] | 杨斌, 彭省临, 李水如, 等. 广西有色金属成矿系列与成矿区带[J]. 矿产与地质, 2007, 21(1):8-11. |
[18] | 崔彬, 翟裕生, 蒙义峰, 等. 广西大瑶山—西大明山金银成矿系统研究[J]. 地球科学, 2000, 25(4):352-355,396. |
[19] | 柴明春, 付伟, 冯佐海, 等. 广西西大明山弄屯铅锌矿床的成矿流体特征及矿床成因指示意义[J]. 矿床地质, 2015, 34(5):948-964. |
[20] | 陆建辉. 西大明山银铅锌金钨铋矿地质特征、成矿规律及成矿模式[J]. 矿产与地质, 2015, 29(5):560-567. |
[21] | 韦昌山, 乐兴文, 肖昌浩, 等. 广西西大明山地区构造-蚀变调查方法总结及找矿预测地质模型构建项目报告[R]. 北京: 中国地质科学院地质力学研究所, 2015:1-264. |
[22] | 张珩清, 付伟, 冯佐海, 等. 广西西大明山罗维矿区层状矽卡岩的发现及成矿意义[J]. 桂林理工大学学报, 2015, 35(4):712-720. |
[23] |
CAROY B, BARBEY P. Ferromagnesian silicate association in S-type granites:the Darongshan granitic complex (Guangxi,South China)[J]. Bulletin de la Societe Geologique de France, 2008, 179(1):13-27.
DOI URL |
[24] |
CHEN C H, HSIEH P S, LEE C Y, et al. Two episodes of the Indosinian thermal event on the South China Block:constraints from LA-ICPMS U-Pb zircon and electron microprobe monazite ages of the Darongshan S-type granitic suite[J]. Gondwana Research, 2011, 19(4):1008-1023.
DOI URL |
[25] |
DENG J, WANG Q F, LI G J, et al. Tethys tectonic evolution and its bearing on the distribution of important mineral deposits in the Sanjiang region,SW China[J]. Gondwana Research, 2014, 26(2):419-437.
DOI URL |
[26] | 乔龙. 右江盆地及其周缘地区构造演化及铝土矿成矿作用[D]. 北京: 中国地质大学(北京), 2016:1-165. |
[27] |
CAI J X, ZHANG K J. A new model for the Indochina and South China collision during the Late Permian to the Middle Triassic[J]. Tectonophysics, 2009, 467(1/4):35-43.
DOI URL |
[28] |
LIU X F, WANG Q F, ZHANG Q Z, et al. Transformation from Permian to Quaternary bauxite in southwestern South China Block driven by superimposed orogeny:A case study from Sanhe ore deposit[J]. Ore Geology Reviews, 2017, 90:998-1017.
DOI URL |
[29] |
LAPIERRE H, JAHN B M, CHARVET J, et al. Mesozoic felsic arc magmatism and continental olivine tholeiites in Zhejiang province and their relationship with the tectonic activity in southeastern China[J]. Tectonophysics, 1997, 274(4):321-338.
DOI URL |
[30] | 毛景文, 谢桂青, 李晓峰, 等. 华南地区中生代大规模成矿作用与岩石圈多阶段伸展[J]. 地学前缘, 2004, 11(1):45-55. |
[31] |
周永章, 郑义, 曾长育, 等. 关于钦-杭成矿带的若干认识[J]. 地学前缘, 2015, 22(2):1-6.
DOI |
[32] | 朱革非. 广西西大明山隐伏构造、隐伏岩体及其与矿产分布的关系[J]. 地质与勘探, 1989, 12(1):15-17. |
[33] |
LIU Y S, HU Z C, GAO S, et al. In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard[J]. Chemical Geology, 2008, 257:34-43.
DOI URL |
[34] |
LIU Y S, GAO S, HU Z C, et al. Continental and oceanic crust recycling-induced melt-peridotite interactions in the Trans-North China Orogen:U-Pb dating, Hf isotopes and trace elements in zircons of mantle xenoliths[J]. Journal of Petrology, 2010, 51:537-571.
DOI URL |
[35] | LUDWIG K R. Isoplot V.3.0:A Geochronological Toolkit for Microsoft Excel[M]. Berkeley:Berkeley Geochronology Center,Special Publication, 2003, 4:1-70. |
[36] |
BALLARD J R, PALIN J M, CAMPBELL I H, Relative oxidation states of magmas inferred from Ce(IV)/Ce(III) in zircon:application to porphyry copper deposits of northern Chile[J]. Contributions to Mineralogy and Petrology, 2002, 144:347-364.
DOI URL |
[37] | 冯佐海, 付伟, 李赛赛, 等. 广西西大明山银铅锌多金属矿成矿规律与成矿预测[R]. 桂林: 桂林理工大学, 2016:1-267. |
[38] | 谭俊, 魏俊浩, 李水如, 等. 广西昆仑关A型花岗岩地球化学特征及构造意义[J]. 地球科学——中国地质大学学报, 2008, 33(6):743-754. |
[39] | 王登红, 陈毓川, 陈文, 等. 广西南丹大厂超大型锡多金属矿床的成矿时代[J]. 地质学报, 2004, 78(1):132-138,146. |
[40] |
SCHERER E E, CAMERON K L, BLICHERT J T. Lu-Hf garnet geochronology:Closure temperature relative to the Sm-Nd system and the effects of trace mineral inclusions[J]. Geochimica et Cosmochimica Acta, 2000, 64(19):3413-3432.
DOI URL |
[41] |
GRIFFIN W L, PEARSON N J, BELOUSOVA E, et al. The Hf isotope composition of cratonic mantle:LA-MC-ICPMS analysis of zircon megacrysts in kimberlites[J]. Geochimica et Cosmochimica Acta, 2000, 64(1):133-147.
DOI URL |
[42] |
BELOISOVA B A, GRIFFIN W L, O’REILLY S Y. Zircon crystal morphology,trace element signatures and Hf isotope composition as a tool for petrogenetic modeling:Examples from Eastern Australian granitiods[J]. Journal of Petrology, 2006, 47(2):329-353.
DOI URL |
[43] | 李巍, 毕诗健, 杨振, 等. 桂东大瑶山南缘社山花岗闪长岩的锆石U-Pb年龄及Hf同位素特征:对区内加里东期成岩成矿作用的制约[J]. 地球科学——中国地质大学学报, 2015, 40(1):17-33. |
[44] | 李献华, 李正祥, 葛文春, 等. 华南新元古代花岗岩的锆石U-Pb年龄及构造意义[J]. 矿物岩石地球化学通报, 2001, 20(4):271-273. |
[45] |
LI Z X, LI X H, ZHOU H W, et al. Grenvillian continental collision in South China:New SHRIMP U-Pb zircon results and implications for the configuration of Rodinia[J]. Geology, 2002, 30(2):163-166.
DOI URL |
[46] |
CHENG Y B, MAO J W. Age and geochemistry of granites in Gejiu area, Yunnan province,SW China:Constraints on their petrogenesis and tectonic[J]. Lithos, 2010, 120:258-276.
DOI URL |
[47] |
CHEN Z C, LIN W, FAURE M, et al. Geochronolgy and isotope analysis of the Paleozoic to Mesozoic granitoids from northeastern Vietnam and implication for the evolution of the South China block[J]. Journal of Asian Earth Sciences, 2014, 86:131-150.
DOI URL |
[48] | 黄文龙, 许继峰, 陈建林, 等. 云南个旧杂岩体年代学与地球化学:岩石成因和幔源岩浆对锡成矿贡献[J]. 岩石学报, 2016, 32(8):2330-2346. |
[49] |
CHENG Y B, MAO J W, SPANDLER C. Petrogenesis and geodynamic implication of the Gejiu igneous complex in the western Cathaysia block,South China[J]. Lithos, 2013, 175/176:213-229.
DOI URL |
[50] |
XU B, JIANG S Y, WANG R, et al. Late Cretaceous granites from the giant Dulong Sn-polymetallic ore district in Yunnan Pro-vince, South China:Geochronology,geochemistry,mineral chemistry and Nd-Hf isotopic compositions[J]. Lithos, 2015, 218/219:54-72.
DOI URL |
[51] |
CHEN X C, HU R Z, BI X W, et al. Zircon U-Pb ages and Hf-O isotopes,and whole-rock Sr-Nd isotopes of the Bozhushan granite,Yunnan province,SW China:Constraints on petrogene-sis and tectonic setting[J]. Journal of Asian Earth Sciences, 2015, 99:57-71.
DOI URL |
[52] | 刘艳宾, 莫宣学, 张达, 等. 滇东南老君山地区晚白垩世花岗岩的成因[J]. 岩石学报, 2014, 30(11):3271-3286. |
[53] |
ZHOU X Y, YU J H, O’REILLY S Y, et al. Sources of the Nanwenhe-Song Chay granitic complex (SW China-NE Vietnam)and its tectonic significance[J]. Lithos, 2017, 290/291:76-93.
DOI URL |
[54] |
BOLHAR R, WEAVER S D, PALIN J M, et al. Systematics of zircon crystallisation in the Cretaceous separation point suite,New Zealand,using U-Pb isotope,REE and Ti geothermometry[J]. Contributions to Mineralogy Petrology, 2008, 156(2):133-160.
DOI URL |
[55] |
BURHAM A D, BERRY A J. An experimental study of trace ele-ment partitioning between zircon and melt as a function of oxygen fugacity[J]. Geochimica et Cosmochimica Acta, 2012, 95:196-212.
DOI URL |
[56] |
TRAIL D, WATSON B E, TAILBY N D. Ce and Eu anomalies in zircon as proxies for the oxidation state of magmas[J]. Geochimica et Cosmochimica Acta, 2012, 97:70-87.
DOI URL |
[57] |
SHEN P, KEIKO H, HONGDI P, et al. Oxidation condition and metal fertility of granitic magmas:Zircon trace-element data from porphyry Cu deposits in the central Asian orogenic belt[J]. Economic Geology, 2015, 110:1861-1878.
DOI URL |
[58] |
CHENG Y B, MAO J W, LIU P. Geodynamic setting of Late Cretaceous Sn-W mineralization in southeastern Yunnan and northeastern Vietnam[J]. Solid Earth Sciences, 2016, 1(3):79-88.
DOI URL |
[59] | 颜丹平, 周美夫, 王焰, 等. 都龙—Song Chay变质穹隆体变形与构造年代——南海盆地北缘早期扩张作用始于华南地块张裂的证据[J]. 地球科学——中国地质大学学报, 2005, 30(4):402-412. |
[60] | 王东升, 刘俊来, MYDUNG T, et al. 越南东北部静足(Tĩnh Túc)钨锡矿区花岗岩年代学、地球化学与区域构造意义[J]. 岩石学报, 2011, 27(9):2795-2808. |
[61] |
CAI J X, ZHANG K J. A new model for the Indochina and South China collision during the Late Permian to the Middle Triassic[J]. Tectonophysics, 2009, 467(1/4):35-43.
DOI URL |
[1] | 刘青占, 蒋孝君, 王果, 李天瑜, 李东鹏. 内蒙古南炮台花岗斑岩成因与构造环境:锆石U-Pb年代学、Hf同位素和全岩元素组成制约[J]. 现代地质, 2024, 38(01): 154-168. |
[2] | 杨元江, 邓昌州, 李成禄, 杨文鹏, 符安宗, 郑博, 袁茂文, 张立东. 小兴安岭翠峦地区早侏罗世A型花岗岩成因与动力学背景[J]. 现代地质, 2023, 37(06): 1597-1608. |
[3] | 梁乾坤, 陈岳龙, 王善辉, 于洋, 杨帆. 嫩江河漫滩沉积物碎屑锆石U-Pb年龄、Hf同位素组成及其地质意义[J]. 现代地质, 2023, 37(03): 529-546. |
[4] | 薛仲凯, 范堡程, 黄豪擎, 唐卫东, 葛战林, 李朋伟, 胡建辉, 杨晓奇, 郭永超, 李空. 内蒙古北山地区中基性岩脉年代学和地球化学特征:对塔里木板块北缘构造演化的启示[J]. 现代地质, 2023, 37(03): 627-644. |
[5] | 邓科, 王金贵, 董玉杰, 何林武, 袁仁华, 张泽国, 陈守关, 辛堂. 西藏桑耶地区晚白垩世中性侵入岩的成因及对新特提斯板块北向俯冲的指示意义[J]. 现代地质, 2023, 37(02): 375-389. |
[6] | 任程昊, 佘宏全, 柯昌辉, 孙衍东, 周群茂, 焦天龙, 李保亮. 福建平和钟腾铜矿床成岩成矿时代研究[J]. 现代地质, 2022, 36(06): 1447-1464. |
[7] | 吕云鹤, 董国臣, 赵丽玮, 苏麟, 殷国栋, 汤家辉. 内蒙古沙章土矿区闪长玢岩成岩时代及岩浆源区探讨:锆石U-Pb年代学、岩石地球化学及Hf同位素约束[J]. 现代地质, 2022, 36(03): 836-847. |
[8] | 刘建栋, 李五福, 王国良, 董进生, 曹锦山, 李红刚, 赵忠国. 北祁连东段柏木峡—门岗峡地区蛇绿岩的识别及其区域构造意义[J]. 现代地质, 2022, 36(01): 244-258. |
[9] | 李秀章, 王立功, 李衣鑫, 王英鹏, 于晓卫, 张文, 郭瑞朋, 刘汉栋. 胶东艾山岩体二长花岗岩地球化学、锆石U-Pb年代学及Lu-Hf同位素特征研究[J]. 现代地质, 2022, 36(01): 333-346. |
[10] | 谢亘, 喻光明, 路英川, 冯欣, 田光昊, 王然, 王建. 华北克拉通南缘小秦岭地区花岗质片麻岩年代学和地球化学特征及其地质意义[J]. 现代地质, 2021, 35(06): 1702-1712. |
[11] | 王玉平, 吴文彬, 刘永俊, 李海洋, 王晓亮, 李超. 辽东岫岩地区晚侏罗世侵入岩的年代学、地球化学特征及地质意义[J]. 现代地质, 2021, 35(04): 955-967. |
[12] | 张宇, 唐名鹰, 崔霄峰, 何玉良, 董卫东. 西昆仑东段苏巴什洋向北俯冲:来自早—中二叠世火山岩的证据[J]. 现代地质, 2021, 35(03): 763-775. |
[13] | 何泽宇, 申俊峰, 张善明, 刘俊, 杜佰松. 内蒙古乌海桌子山花岗岩的锆石U-Pb年代学、地球化学特征及其地质意义[J]. 现代地质, 2021, 35(02): 523-534. |
[14] | 于立栋, 于学峰, 李大鹏, 刘强, 刘家军, 舒磊, 尉鹏飞. 鲁西临朐铁寨杂岩体锆石U-Pb年代学、地球化学特征及其地质意义[J]. 现代地质, 2020, 34(03): 418-430. |
[15] | 张云, 孙立新, 张天福, 孙义伟, 张祺, 李艳锋, 杨泽黎, 刘文刚. 内蒙古狼山地区乌花辉长岩的年代学、地球化学和Sr-Nd-Hf同位素组成:对地幔源区特征和岩石成因的约束[J]. 现代地质, 2020, 34(03): 450-465. |
阅读次数 | ||||||
全文 |
|
|||||
摘要 |
|
|||||