地球科学进展

地球科学进展 ›› 2015, Vol. 30 ›› Issue (9): 1034 -1049. doi: 10.11867/j.issn.1001-8166.2015.09.1034

上一篇    下一篇

中祁连西段花岗岩类的地球化学特征及构造意义
侯荣娜 1( ), 王淑华 1, 张翔 2, 侯克选 1, 张铖 3, 王金荣 1, *( )   
  1. 1.兰州大学地质科学与矿产资源学院 甘肃省西部矿产资源重点实验室(兰州大学),甘肃 兰州 730000
    2.甘肃省地质调查院,甘肃 兰州 730000
    3.甘肃省地质矿产开发局第二勘查院,甘肃 兰州 730000
  • 收稿日期:2015-07-15 修回日期:2015-08-27 出版日期:2015-09-20
  • 通讯作者: 王金荣 E-mail:hourn09@lzu.edu.cn;jrwang@lzu.edu.cn
  • 基金资助:
    甘肃省科技重大专项计划项目“祁连山造山带西段石板墩铁矿床赋矿层位及找矿预测研究”(编号：1002FKDA042);中央高校基本科研业务费专项资金“中祁连西段野马南山火成岩组合及其构造意义”(编号：lzujbky-2013-113)资助

Geochemical Characteristics and Tectonic Significance of the Granotoids in the Western Section of the Mid-Qilian

Rongna Hou 1( ), Shuhua Wang 1, Xiang Zhang 2, Kexuan Hou 1, Cheng Zhang 3, Jinrong Wang 1( )   

  1. 1.Key Laboratory of Mineral Resources in Western China (Gansu Province), School of Earth Sciences, Lanzhou University, Lanzhou 730000, China
    2. Geological Survey of Gansu Province, Lanzhou 730000, China
    3. Second Institute of Geological and Mineral Exploration of Gansu Provincial Bureau of Geology and Mineral Resources, Lanzhou 730000, China
  • Received:2015-07-15 Revised:2015-08-27 Online:2015-09-20 Published:2015-09-20
全文 ( 3 ) 下载PDF ( 1043 )

中祁连西段石板墩地区北部及南部发育有辉长岩、闪长岩及花岗岩。北带岩体的LA-ICP-MS锆石U-Pb年龄为（469.3±2.8）Ma,（461.2±3.3）Ma和（470.0±2.5）Ma;岩石SiO2质量百分含量为53.2%~66.11%,高Al,Ti,Mg,Fe,Ca,K,Na,A/CNK<1.1;富集大离子亲石元素Rb,K和Pb,亏损高场强元素Nb,Ta,Ce,Sr,Hf,Ti;REE总量较高,LREE富集、HREE近平坦型分布,中等的负Eu异常,δEu=0.6;此外,在构造判别图中,样品落于岛弧环境。南带岩体LA-ICP-MS锆石U-Pb年龄为（470.9±2.8）Ma和（472.3±4.2）Ma,岩石SiO2质量百分含量较高（67.13%~70.73%）,高Al,Mg,Fe,Ca,富Na贫K,A/CNK<1.1;岩石表现为明显的高Sr低Yb,Y的特点,富集大离子亲石元素R,K,Sr等,亏损高场强元素Nb,Ta,P,Ti等;REE总量较低,LREE富集、HREE亏损,轻重稀土分异明显,轻微的负Eu异常至正异常,δEu=0.74~1.18。研究表明,北带岩体为地幔楔部分熔融产生的,形成于岛弧环境;南带岩体为消减的大洋岩石圈板块部分熔融产生的埃达克岩,是北祁连向南俯冲导致的岩浆作用的产物,“中祁连西段”是早古生代时期在“残留的微陆块”基础上形成的一个岛弧增生杂岩地体。

关键词: 中祁连西段, 岛弧, 埃达克岩, 早古生代

Granotoids, mainly gabbro, diorite and granite, are greatly rich in the northern and southern parts of Shibandun area, western section of the Mid-Qilian. LA-ICP-MS zircon and U-Pb dating methods indicate that the age of the rock from the northern belt were（469.3±2.8）Ma,（461.2±3.3）Ma and (470.0±2.5) Ma, respectively. The SiO2 content of the northern rock mass ranges from 53.2% to 66.1% with high content of the Al, Ti, Mg, Fe, Ca, K, Na in the rock mass and A/CNK<1.1. The rock analysis shows enrichment of large ion lithophile elements (LILE) (e.g., Rb, K) and Pb, and depletion of high field strength elements (HFSE) (e.g., Nb, Ta, Ce, Sr, Hf and Ti). The results also indicate LREE enriched pattern with high ∑REE abundance, flat HREE and moderate negative Eu anomaly (δEu=0.6). Tectonic discrimination diagrams showed that the samples are located in the arc environment. The age of the rock from the southern belt are respectively （470.9±2.8） Ma and （472.3±4.2） Ma based on LA-ICP-MS zircon U-Pb dating methods. The southern rock mass contains high amount of the Al, Mg, Fe, Ca and is rich in Na and poor in K (A/CNK<1.1). Rock analysis results show the enrichment of large ion lithophile elements (LILE) (e.g., Rb, K and Sr) and depletion of high field strength elements (HFSE) (e.g., Nb, Ta, Ti and P), and also indicate a LREE enriched pattern with rather low ∑REE, depleted HREE and obvious differentiation in Eu, which is from slight negative to positive anomaly (δEu=0.74~1.18). Our study shows that the northern belt was formed by partial melting of mantle wedge in an island-arc environment, while the southern belt is adakites generated by partial melting of Adakites, and is also the product from the magmatic process by the North Qilian southward subduction. The western part of the Mid-Qilian is an island arc hyperplasia complex created on a remained microcontinental in early Paleozoic.

Key words: The western section of the Mid-Qilian, Island arc, Adakites, Early Paleozoic.

中图分类号: 

图1 研究区区域地质构造图 1:第四系;2:新近系;3:古近系;4:寒武系;5:青白口系哈什哈尔组;6:青白口系五个山组;7:蓟县系花儿地组c岩组;8:蓟县系花儿地组b岩组;9:蓟县系南白水河组;10:长城系南白水河组;11:肉红色中细粒花岗岩;12:灰白色花岗闪长岩;13:灰绿色中细粒英云闪长岩;14:玄武安山岩;15:辉长岩;16:橄辉岩;17:不整合界线;18:逆断层;19:正断层;20:实测性质不明断层;21:采样点
Fig.1 Regional tectonic map of the studied area 1：Quaternary System; 2: Neogene System; 3:Paleogene System; 4: Cambrian System; 5: Qingbaikou System Hashihar Fm; 6:Qingbaikou System Wugeshan Fm; 7: Jixian System Huaerdi Fm c rock group; 8: Jixian System Huaerdi Fm b rock group; 9:Jixian System Nanbaishuihe Fm; 10:Changcheng System Nanbaishuihe Fm; 11:Fine-Medium grained granite in flesh pink; 12: Gray granite diorite; 13: Fine-Medium Tonalite in celadon; 14: Basaltic Andesite; 15: Gabbro; 16: Peridotite; 17: Unconformity Boundary; 18: Thrust fault; 19: Normal fault; 20: The measured properties unknown fault; 21: Sampling points
表1 岩石LA-ICP-MS锆石U-Pb年龄分析结果
Table 1 Dating of the Zircon LA-ICP-MS U-Pb age of the rocks
样品号及 Pb Th U Th/U 同位素比值 表面年龄
分析点号 ×10-6 207Pb/235U 1σ 206Pb/238U 1σ 207Pb/235U 1σ 206Pb/238U 1σ
YQ6-01 114.72 136.06 351.23 0.387 0.59048 0.01357 0.07536 0.00098 471 9 468 6
YQ6-02 107.01 190.14 324.63 0.586 0.57939 0.01372 0.07406 0.00097 464 9 461 6
YQ6-03 74.38 80.15 223.21 0.359 0.58162 0.01405 0.07727 0.00103 466 9 480 6
YQ6-04 62.39 121.05 180.33 0.671 0.60265 0.01635 0.07719 0.00105 479 10 479 7
YQ6-05 50.16 81.63 146.74 0.556 0.59809 0.02621 0.07705 0.00122 476 17 478 8
YQ6-06 109.92 133.69 339.49 0.394 0.57524 0.01289 0.07471 0.00098 461 8 464 6
YQ6-07 54.79 69.52 165.84 0.419 0.59555 0.02026 0.07586 0.00107 474 13 471 6
YQ6-08 88.91 195.4 257.21 0.76 0.59613 0.01453 0.07649 0.00102 475 9 475 6
YQ6-09 55.29 96.74 160.88 0.601 0.6085 0.01819 0.07746 0.00107 483 11 481 7
YQ6-10 51.13 87.78 147.76 0.594 0.64161 0.02021 0.07747 0.00108 503 13 481 8
YQ6-11 76.72 125.47 229.5 0.547 0.59915 0.01647 0.07595 0.00102 477 10 472 6
YQ6-12 56.31 91.49 165.76 0.552 0.61131 0.02024 0.07708 0.00108 484 13 479 8
YQ6-13 43.91 71.36 130.52 0.547 0.59172 0.01767 0.07624 0.00107 472 11 474 7
YQ6-14 72.03 161 214.96 0.749 0.57073 0.0149 0.07446 0.00101 458 10 463 6
YQ6-15 73.05 163.95 223.23 0.734 0.55973 0.0146 0.07245 0.00098 451 10 451 6
YQ6-16 66.4 125.77 196.3 0.641 0.60959 0.01775 0.07591 0.00103 483 11 472 7
YQ6-17 87.42 174.66 260.6 0.67 0.58592 0.01432 0.07527 0.001 468 9 468 6
YQ6-18 61.65 109.54 183.78 0.596 0.5923 0.01703 0.07595 0.00104 472 11 472 6
YQ6-19 56.99 114.74 168.44 0.681 0.59276 0.01715 0.07582 0.00105 473 11 471 6
YQ6-20 74.3 89.28 227.89 0.392 0.59039 0.01621 0.07558 0.00102 471 10 470 6
YQ6-21 76.48 143.16 229.37 0.624 0.58752 0.01598 0.07523 0.00102 469 10 468 6
YQ6-22 65.98 96.77 194.3 0.498 0.57881 0.01648 0.07443 0.00102 464 11 463 7
YQ6-23 85.45 147.92 258.01 0.573 0.58618 0.01498 0.07515 0.00101 468 10 467 6
YQ6-24 61.96 133.17 182.19 0.731 0.59104 0.01717 0.07582 0.00105 472 11 471 6
YQ6-25 49.51 78.48 149.84 0.524 0.58566 0.01788 0.07532 0.00106 468 11 468 7
YQ6-26 63.37 100.56 187.56 0.536 0.54618 0.0151 0.07371 0.00101 442 10 458 6
YQ6-27 41.514 64.02 122.01 0.525 0.60295 0.01844 0.0779 0.0011 479 12 484 8
YQ6-28 68.04 124.6 205.74 0.606 0.58369 0.01703 0.07438 0.00102 467 11 462 6
YQ6-29 63.4 96.37 189.53 0.508 0.63882 0.01796 0.07598 0.00104 502 11 472 6
YQ6-30 91.37 99.89 286.73 0.348 0.59788 0.01537 0.0741 0.00099 476 10 461 6
YQ10-01 238.41 539.16 698.35 0.772048 0.58316 0.01331 0.07505 0.00098 466 9 467 6
YQ10-02 135.91 244.81 407.33 0.601011 0.58349 0.01458 0.07508 0.001 467 9 467 6
YQ10-03 141.23 301.78 417.6 0.722653 0.58507 0.01516 0.07467 0.001 468 10 464 8
YQ10-04 228.06 347.61 713.06 0.487491 0.56249 0.01206 0.0728 0.00094 453 8 453 6
YQ10-06 158.36 267.74 490.26 0.546118 0.56578 0.01342 0.07304 0.00097 455 9 454 6
YQ10-07 271.8 761.37 773.93 0.983771 0.60775 0.01277 0.07618 0.00099 482 8 473 6
YQ10-09 144.93 232.18 441.94 0.525365 0.58661 0.01337 0.0743 0.00097 469 9 462 6
YQ10-11 151.08 272.53 461.7 0.590275 0.59106 0.01501 0.07347 0.00098 472 10 457 8
YQ10-12 519.95 2079.92 1429.93 1.454561 0.59676 0.01235 0.07608 0.00098 475 8 473 6
YQ10-13 100.71 141.46 300.92 0.470092 0.59801 0.0168 0.07632 0.00105 476 11 474 8
YQ10-14 129.9 209.31 393.07 0.532501 0.58428 0.01564 0.075 0.00102 467 10 466 8
YQ10-15 112.37 110.88 340.05 0.32607 0.59984 0.01915 0.07682 0.00109 477 12 477 7
YQ10-16 211.76 464.55 639.98 0.725882 0.58098 0.01361 0.07374 0.00097 465 9 459 6
YQ10-17 238.44 381.31 743.37 0.512948 0.57954 0.0126 0.07294 0.00095 464 8 454 6
YQ10-18 274.06 670.04 827.57 0.809648 0.57188 0.01297 0.07276 0.00095 459 8 453 6
YQ10-19 113.17 181.25 350.77 0.51672 0.57565 0.01526 0.07342 0.00099 462 10 457 7
YQ10-20 222.11 454.21 665.59 0.682417 0.61198 0.01449 0.07406 0.00098 485 9 461 6
YQ10-24 110.68 194.14 331.6 0.585464 0.58379 0.01589 0.0753 0.00102 467 10 468 7
YQ10-25 216.02 248.4 670.1 0.370691 0.58093 0.01312 0.07456 0.00098 465 8 464 6
YQ10-27 242.75 510.02 719.71 0.708647 0.58979 0.01304 0.07441 0.00097 471 8 463 6
YQ10-29 172.71 334.02 523.64 0.637881 0.57359 0.01559 0.07413 0.00101 460 10 461 7
YQ10-30 242.36 551.92 739.94 0.745898 0.56739 0.0137 0.07258 0.00096 456 9 452 6
YQ11-01 161 284.89 487.97 0.583827 0.57884 0.01457 0.07479 0.001 464 9 465 6
YQ11-02 304.67 747.44 871.11 0.858032 0.60645 0.015 0.07669 0.00102 481 9 476 6
YQ11-03 146.19 212.06 441.94 0.479839 0.59248 0.01543 0.07568 0.00102 472 10 470 6
YQ11-04 198.6 468.12 576.56 0.811919 0.59648 0.01444 0.07586 0.00101 475 9 471 6
YQ11-05 218.57 500.99 625.65 0.800751 0.63247 0.01614 0.07698 0.00104 498 10 478 6
YQ11-06 140.55 290.25 421.97 0.687845 0.58096 0.01519 0.07453 0.001 465 10 463 6
YQ11-07 333.39 834.29 962.19 0.867074 0.59308 0.01356 0.07595 0.001 473 9 472 6
YQ11-08 234.99 524.04 682.97 0.767296 0.59531 0.0155 0.07641 0.00103 474 10 475 6
YQ11-09 313.53 816.07 908.95 0.897816 0.61463 0.01475 0.07439 0.00099 486 9 463 6
YQ11-10 205.71 473.53 614.33 0.770807 0.5824 0.01385 0.07408 0.00098 466 9 461 6
YQ11-12 252.33 489.15 726.62 0.673185 0.60562 0.01479 0.07699 0.00103 481 9 478 6
YQ11-13 202.35 418.49 603.57 0.693358 0.62167 0.01466 0.07399 0.00098 491 9 460 6
YQ11-14 276.98 625.91 809.38 0.77332 0.59138 0.01371 0.07569 0.001 472 9 470 6
YQ11-16 386.46 1028.05 1102.78 0.932235 0.61763 0.01442 0.07621 0.00101 488 9 473 6
YQ11-17 169.47 325.53 497.01 0.654977 0.60374 0.01705 0.07646 0.00105 480 11 475 6
YQ11-19 216.89 430.47 638.27 0.674432 0.62603 0.01595 0.07549 0.00102 469 17 467 6
YQ11-21 433.95 1128.09 1231.89 0.915739 0.62814 0.01441 0.07606 0.001 495 9 473 6
YQ11-22 214.18 484.96 625.78 0.774969 0.65989 0.01658 0.07568 0.00102 515 10 470 6
YQ11-23 214.64 392.69 629.86 0.623456 0.59946 0.01523 0.07678 0.00103 477 10 477 6
YQ11-28 132.2 227.64 394.38 0.57721 0.59779 0.01703 0.07603 0.00105 476 11 472 6
YQ11-29 259.62 592.8 778.64 0.761327 0.57377 0.01437 0.07415 0.001 460 9 461 6
YQ11-30 190.48 395.77 562.36 0.703766 0.59584 0.01581 0.07583 0.00103 475 10 471 6
YQ26-01 395.52 369.87 1192.22 0.310236 0.68272 0.01703 0.07703 0.00104 502 13 476 8
YQ26-02 95.96 97.73 295.4 0.33084 0.59997 0.0177 0.07616 0.00106 477 11 473 6
YQ26-03 535.15 1680.58 1544.15 1.088353 0.58422 0.01468 0.0746 0.001 467 9 464 6
YQ26-04 824.68 988.78 2551.21 0.387573 0.61135 0.01515 0.07483 0.00101 484 10 465 6
YQ26-06 95.98 90.33 297.37 0.303763 0.59446 0.01784 0.07605 0.00107 474 11 473 7
YQ26-07 430.26 471.05 1324.4 0.35567 0.59684 0.01529 0.07602 0.00103 475 10 472 6
YQ26-08 121.3 101.1 379.13 0.266663 0.58907 0.01758 0.07576 0.00106 470 11 471 6
YQ26-09 162.06 173.58 491.42 0.353221 0.60386 0.01702 0.07726 0.00107 480 11 480 6
YQ26-10 116.67 127.64 360.7 0.353867 0.59698 0.01826 0.07578 0.00107 475 12 471 8
YQ26-11 143.6 175.75 440.95 0.398571 0.59552 0.01682 0.07583 0.00105 474 11 471 6
YQ26-13 490.28 655.2 1505.47 0.435213 0.59045 0.01517 0.07574 0.00103 471 10 471 6
YQ26-14 195.41 208.46 596.3 0.349589 0.58971 0.01691 0.07535 0.00105 471 11 468 7
YQ26-16 137.75 135.84 427.69 0.317613 0.58864 0.01674 0.07581 0.00105 470 11 471 6
YQ26-17 163.92 217.57 482.66 0.450773 0.59043 0.01738 0.07609 0.00106 471 11 473 6
YQ26-18 74.5 99.43 228.72 0.434724 0.59272 0.02078 0.0757 0.0011 473 13 470 8
YQ26-19 183.06 185.8 569.35 0.326337 0.59332 0.01685 0.07564 0.00105 473 11 470 7
YQ26-20 356.68 356.57 1123.11 0.317484 0.58925 0.01574 0.0748 0.00102 470 10 465 6
YQ26-23 217.12 193.73 658.43 0.29423 0.61345 0.01753 0.07794 0.00108 486 11 484 7
YQ26-25 463.24 894.24 1423.65 0.628132 0.60658 0.01655 0.07363 0.00101 481 10 458 6
YQ26-26 520.94 531.67 1627.18 0.326743 0.59405 0.01609 0.0755 0.00104 473 10 469 6
YQ26-29 220.59 259.59 691.87 0.375201 0.60449 0.01807 0.07442 0.00105 480 11 463 7
YQ26-30 120.08 138.68 370.14 0.374669 0.59275 0.01869 0.07585 0.00108 473 12 471 8
YQ27-01 277.17 707.82 811.08 0.872688 0.61932 0.01849 0.0758 0.00107 489 12 471 6
YQ27-08 149.06 357.85 434.99 0.822663 0.62553 0.02214 0.07662 0.00114 493 14 476 7
YQ27-09 315.23 543.76 953.58 0.57023 0.6029 0.01806 0.0757 0.00107 479 11 470 6
YQ27-13 449.02 761.88 1358.94 0.560643 0.61181 0.01854 0.07622 0.00108 485 12 474 6
YQ27-15 433.07 388.6 1324.27 0.293445 0.63639 0.01904 0.07651 0.00108 500 12 475 6
YQ27-20 328.92 674.83 927.05 0.727933 0.8584 0.02702 0.07641 0.0011 600 23 472 7
YQ27-21 464.38 430.83 1386.2 0.310799 0.69787 0.02237 0.07692 0.00111 485 17 473 7
YQ27-23 261.69 421.98 771.49 0.546968 0.70849 0.02546 0.07703 0.00116 520 21 476 7
YQ27-28 351.86 701.52 939.58 0.746631 0.9806 0.03287 0.07809 0.00116 569 28 473 7
表2 中祁连西段花岗岩类的地球化学成分(主量元素：质量百分含量,%,微量与稀土元素：×10 -6)
Table.2 The geochemical composition of the western section of the Central Qilian granitoid rock（Major element: weight, %; Trace and REE element:×10 -6)
样号 YQ-6 YQ-9 YQ-10 YQ-11 YQ-26 YQ-27
元素 闪长岩 辉长岩 正长花岗岩 花岗闪长岩 花岗闪长岩 花岗岩
SiO2 53.2 51.56 61.67 66.11 67.13 70.73
Al2O3 16.97 17.4 16.97 15.58 16.42 15.86
TiO2 2 1.98 0.92 0.8 0.45 0.31
TFe2O3 11.58 12.09 6.32 5.14 3.39 2.31
MnO 0.19 0.21 0.09 0.08 0.06 0.04
MgO 3.32 3.16 1.36 1.09 2.34 1.17
Ca0 6.01 6.35 4.08 2.91 4.61 2.97
Na2O 4.31 4.22 4.26 3.91 4.01 4.67
K2O 1.83 1.99 4.02 4.1 1.53 1.85
P2O5 0.61 1.04 0.3 0.29 0.06 0.08
Mg# 36.21 34.1 29.83 29.69 57.77 50.11
Li 12.2 15.96 34.24 30.5 35.16 25.46
Sc 24.14 26.2 11.87 9.59 9.38 4.55
Ti 12125.8 14806 5504.08 5414 2834.8 1910.57
V 192.9 135.58 95.01 59.68 90.26 56.19
Cr 22.22 55.34 5.71 5.22 21.58 8.38
Co 23.12 25.72 10.01 8.57 11.89 5.56
Ni 15.55 36.98 6.04 7.39 14.51 5.63
Cu 34.68 42.78 23.55 18.52 20.28 1.57
Zn 119.26 136.86 77.71 66.96 36.48 41.72
Ga 27.26 29.94 22.65 21.16 16.57 16.61
Rb 71.24 86.76 174.1 175.24 57.24 61.1
Sr 272.2 311 175.44 173.24 399.6 386.57
Zr 332.4 499.14 444.9 328.14 54.46 106.04
Nb 21.44 29.61 16.44 20.02 4.56 7.08
Cs 2.38 1.84 6.89 6.22 3.28 2.77
Ba 490.8 625.4 738.19 641 453 418.88
Hf 8.28 9.42 11.82 7.1 1.33 2.61
Ta 1.04 1.8 0.99 1.63 0.36 0.49
Pb 8.41 6.52 17.19 16.32 11.66 14.58
Th 3.84 1.76 13.7 11.74 5.85 6.99
U 0.89 0.98 1.99 1.76 1.14 1.39
La 32.12 33.34 38.41 31.9 8 22.02
Ce 73.86 84.54 77.94 64.7 15.64 37.63
Pr 10.2 11.34 9.62 7.6 1.99 3.89
Nd 42.82 51.18 36.57 30.14 7.72 12.37
Sm 10.29 12.59 7.95 6.54 2.13 1.88
Eu 2.76 3.3 1.65 1.34 0.53 0.64
Gd 11.27 13.6 8.12 6.63 2.25 1.47
Tb 1.76 2.14 1.24 1.04 0.35 0.18
Dy 11.03 13.24 7.78 6.39 2.11 0.96
Ho 2.21 2.67 1.54 1.3 0.39 0.17
Er 6.37 7.57 4.48 3.76 1.1 0.5
Tm 0.98 1.05 0.69 0.54 0.16 0.07
Yb 5.99 6.72 4.31 3.54 1 0.46
Lu 0.89 0.99 0.64 0.53 0.14 0.07
Y 74.36 66.16 53.38 32.5 13.75 6.3
∑REE 286.9 310.43 254.34 198.43 57.24 88.62
LREE 172.05 196.28 172.14 142.22 36 78.44
HREE 114.85 114.15 82.2 56.2 21.24 10.18
δEu 0.78 0.77 0.63 0.62 0.74 1.18
δCe 1 1.07 0.99 1.02 0.96 1
La/Sm 3.12 2.65 4.83 4.88 3.76 11.74
Sm/Nd 0.24 0.25 0.22 0.22 0.28 0.15
(La/Yb)N 3.85 3.56 6.39 6.47 5.76 34.19
图2 选择的部分锆石阴极发光（CL）影像图
Fig.2 Zircon cathodoluminescence (CL) images
图3 样品YQ-6,YQ-10,YQ-11,YQ-26,YQ-27 LA-ICP-MS锆石U-Pb年龄谐和图
Fig. 3 YQ-10,YQ-11,YQ-26,YQ-27 LA-ICP-MS U-Pb zircon concordia diagram
图4 石板墩地区中酸性岩SiO 2-Na 2O+K 2O图解 [ 70 ]
Fig. 4. SiO 2-Na 2O+K 2O(TAS) diagram foracid-intermediate rock [ 70 ]
图5 岩石SiO 2-K 2O图解 [ 71 ]
Fig.5 SiO 2-K 2O diagram of rocks [ 71 ]
图6 花岗岩类A/NK-A/CNK图解 [ 72 ]
Fig.6 Diagrams of A/NK-A/CNK [ 72 ]
图7 石板墩地区花岗岩类微量元素蛛网图及稀土元素配分图 [ 73 ]
Fig.7. Primary mantle-normalized trace element spider diagram and chondrite-normalized REE patterns for acgranitoid rock [ 73 ]
图8 花岗岩类构造环境判别图解 [ 74 ]
Fig. 8 Discrimination diagrams of tectonic setting of granitoid [ 74 ]
图9 花岗岩Sr/Y-Y和(La/Yb) N-Yb N图解 [ 77 , 81 ] Sr/Y-Y中1:榴辉岩（石榴石/辉石=50/50）; 2:角闪石榴岩（石榴石/角闪石=50/50）;3:角闪榴辉岩（角闪石/石榴石/辉石=10/40/50）;4:石榴角闪岩（石榴石/角闪石=10/90）
Fig.9 Plot of Sr/Y versus Y and (La/Yb) N versus Yb N diagrams [ 77 , 81 ] In Sr/Y,1: eclogite(garnet/pyroxene=50/50);2: hornblende garnet rock（garnet/homblende）=50/50);3: amphibole eclogite (homblende/garnet/pyroxene=10/40/50);4: garnet amphibolite(garnet/homblende=10/90)
图10
Fig.10 SiO 2-MgO diagram for acid-intermediate rock [ 82 ] Adakite in the east of China and the Pacific rim accorded reference [ 83 ]
图11 北祁连大洋构造演化模式简图（据参考文献[ 88 ]修改）
Fig.11 Tectonic evolution model of North Qilian ocean（Modified according to [ 88 ]）
[37] Wang Erqi,Zhang Qi, Burchfiel C B.The Lajishan Fault Belt in Qinghai Province:A multi-staged uplifting structural window[J]. Scientia Geologica Sinica, 2000, 35(4): 493-500.
[王二七, 张旗, Burchfiel C B.青海拉鸡山: 一个多阶段抬升的构造窗[J]. 地质科学, 2000, 35(4): 493-500.]
[38] Su Jianping, Hu Nenggao, Fu Guomin.High-pressure metamorphism of granet-bearing amohibolite in the Gongchakou region, Western Qilian Mountains and its geological implication[J]. Acta Mineralogica Sinica, 2004, 24(4):391-397.
[苏建平,胡能高,付国民.祁连西段龚岔口地区榴闪岩的高压变质作用及其地质意义[J].矿物学报,2004, 24(4):391-397.]
[39] Su Jianping,Hu Nenggao, Zhang Haifeng, et al.U-Pb Zircon dating and genesis of the Heigouliangzi granitic intrusion in the western segment of the Middle Qilian Mountains[J].Geoscience, 2004, 18(1):70-74.
[苏建平,胡能高,张海峰,等.中祁连西段黑沟梁子花岗岩的锆石U-Pb同位素年龄及成因[J].现代地质,2004, 18(1):70-74.]
[40] Su Jianping, Zhang Xinhu, Hu Nenggao,et al.Geochemical characteristics and genesis of adakite-like granites at Yema Nanshan in the western segment of the Central Qilian Mountains[J]. Geology in China,2004,31(4):365-371.
[苏建平,张新虎,胡能高,等.中祁连西段野马南山埃达克质花岗岩的地球化学特征及成因[J].中国地质,2004,31(4):365-371.]
[41] Li JianFeng, Zhang Zhicheng, Han Baofu. Geochronology and geochemistry of Early Paleozoic granitic plutons from Subei and Shibaocheng areas, the western segment of Central Qilian and their geological implications[J]. Acta Petrologica Sinica,2010,26(8):2 431-2 444.
[李建锋,张志诚,韩宝福.中祁连西段肃北、石包城地区早古生代花岗岩年代学、地球化学特征及其地质意义[J].岩石学报,2010,26(8):2 431-2 444.]
[1] Wang Quan, Liu Xueya.Paleo-oceanic crust of the Chilienshan religion, western China and its tectonic significance[J]. Acta Geologica Sinica,1976,1:42-55.
[王荃, 刘雪亚.我国西部祁连山区的古海洋地壳及其大地构造意义[J].地质学报,1976,1:42-55.]
[2] Xiao Xuchang, Chen Guoming, Zhu Zhizhi.A preliminary study on the tectonics of ancient ophiolites in the Qilian Mountain, northwest of China[J]. Acta Geologica Sinica, 1978,52:287-295.
[肖序常, 陈国铭, 朱志直.祁连山古蛇绿岩带的地质构造意义[J]. 地质学报,1978,52:287-295.]
[3] Feng Yimin, He Shiping.Geotectonics and Orogeny of the Qilian Mountains[M]. Beijing: Geological Publish House, 1996.
[冯益民, 何世平.祁连山大地构造与造山作用[M].北京:地质出版社,1996.]
[4] Zhao Shenggui.The Characteristics of Qilian Orogenic belt and its tectonic evolution[J].Acta Geologica Gansu, 1996,5(1):16-29.
[赵生贵. 祁连造山带特征及其构造演化[J].甘肃地质学报,1996,5(1):16-29.]
[5] Feng Y M, He S P.Orogenic process of the Qilian Mountains[J].Acta Geoscientia Sinica,1996,76(2):1-5.
[6] Wan Yusheng, Xu Zhiqin, Yang Jingsui, et al.The Precambrian high-grade basement of the Qilian terrane and neighboring areas: Its ages and compositions[J].Acta Geoscientia Sinica, 2003,24(4):319-324.
[万渝生,许志琴,杨经绥,等.祁连造山带及邻区前寒武纪深变质基底的时代和组成[J].地球学报,2003,24(4):319-324.]
[7] Lu Songnian, Li Huaikun, Wang Huichu, et al.Detrital zircon population of Proterozoic metasedimantary strata in the Qinling-Qilian-Kunlun Orogen[J]. Acta Petrologica Sinica, 2009,25(9):2 195-2 208.
[陆松年,李怀坤,王惠初,等.秦·祁·昆造山带元古宙副变质岩层碎屑错石年龄谱研究[J].岩石学报,2009,25(9):2 195-2 208.]
[8] Xu Zhiqin,Yang Jingsui,Li Haibing, et al.The early Palaeozoic terrene framework and the formation of the Hhigh-Pressure(HP) and Ultra-High Pressure(UHP) metamorphic belts at the Central Orogenic Belt (COB)[J]. Acta Geologica Sinica, 2006,80(12):1 793-1 806.
[许志琴,杨经绥,李海兵,等.中央造山带早古生代地体构架与高压/超高压变质带的形成[J].地质学报,2006,80(12):1 793-1 806.]
[9] Yang Jingsui, Xu Zhiqin, Ma Changqian, et al.Compound orogeny and scientific problems concerning the Central Orogenic Belt of China[J].Geology in China,2010, 37(1):1-11.
[杨经绥,许志琴,马昌前,等.复合造山作用和中国中央造山带的科学问题[J].中国地质,2010, 37(1):1-11.]
[10] Wang Jinrong, Wu Chunjun, Cai Zhenghong, et al. Early Paleozoic high-Mg adakite from Yindongliang in the eastern section of the North Qilian: Implications for geodynamics and Cu-Au mineralization[J]. Acta Petrologica Sinica, 2006,22(11):2 655-2 664.
[王金荣,吴春俊,蔡郑红,等.北祁连山东段银铜粱早古生代高镁埃达克岩:地球动力学及成矿意义[J].岩石学报,2006,22(11):2 655-2 664.]
[11] Song Shuguang, Niu Yaoling, Su Li, et al. Tectonics of the North Qilian orogen[J].Gondwana Research, 2013,23(4): 1 378-1 401.
[12] Xu Zhiqing, Xu Huifen, Zhang Jianxin, et al.The Zoulangshan Caledonian subductive complex in the Northern Qilian Mountains and its dynamics[J]. Acta Geologica Sinica, 1994,68(1): 1-15.
[许志琴,徐惠芬,张建新,等.北祁连走廊南山加里东俯冲杂岩增生地体及其动力学[J].地质学报,1994,68(1): 1-15.]
[13] Zhang Qi, Sun Xiaomeng, Zhou Dejin,et al.The characteristics of North Qilian opliiolites environment of fomation and their tectonic significance[J].Advances in Earth Science, 1997, 12(4):366-393.
[42] Wang Jinrong, Zhang Xinhu, Zhang Xiang, et al.Tectonics, Rock Combination and petrogenesis of Yema-Nanshan from the western segment of the Central Qilian[C]∥National Symposium on Petrology Geodynamics, 2012:466-468.
[王金荣,张新虎,张翔,等.中祁连西段野马南山构造岩石组合、成因及其构造意义[C]∥全国岩石学与地球动力学研讨会论文摘要集,2012:466-468.]
[43] Dong Guoan,Yang Huairen, Yang Hongyi,et al.SHRIMP U-Pb Zircon geochronology of Precambrian basement from the Qilian massif and their tectonic implications[J]. Chinese Science Bulletin, 2007,52(13):1 572-1 585.
[董国安,杨怀仁,杨宏仪,等.祁连地块前寒武基底锆石SHRIMP U-Pb年代学及其地质意义[J].科学通报,2007,52(13):1 572-1 585.]
[44] Zuo Guochao, Liu Jichen.The evolution of Tectonic of Early Paleozoic in North Qilian Range ,China[J]. Chinese Journal of Geology,1987,(1):14-24.
[左国朝,刘寄陈.北祁连早古生代大地构造演化[J].地质科学,1987,(1):14-24.]
[45] Xia Linqi, Xia Zuchun, Ren Youxiang, et al.The Marine Volcanic Rocks from Qinlin and Qilian Mountains[M].Wuhan: China University of Geosciences Press, 1991.
[夏林圻,夏祖春,任有祥,等.祁连、秦岭山系海相火山岩[M].武汉:中国地质大学出版社,1991.]
[46] Feng Yimin,He Shiping.Ophiolite and orogeny:Annalysis for the northe Qilian orogenie belt as an exemple[M]∥Zhang Qi, ed. Study on Ophiolites and Geodynamics. Beijing: Geological Publish House, 1996:135-138.
[冯益民, 何世平. 蛇绿岩与造山作用——北祁连造山带例析[M]//张旗编. 蛇绿岩与地球动力学研究. 北京: 地质出版社, 1996:135-138.]
[47] Xu Wangchun, Zhang Hongfei, Liu Xiaoming.U-Pb zircon dating constraints on formation time of Qilian high-grade metamorphic rock and its tectonic implications[J]. Chinese Science Bulletin, 2007, 52(4): 531-538.
[徐旺春,张宏飞,刘小明.锆石U-Pb定年限制祁连山高级变质岩系的形成时代及其构造意义[J].科学通报,2007,52(4):531-538.]
[48] Wan Yusheng, Xu Zhiqin, Yang Jingsui, et al.Ages and compositions of the precambrian high-grade basement of the Qilian Terrane and its adjacent areas[J]. Acta Geologica Sinica, 2001,75(4):375-384.
[49] Wan Yusheng, Zhang Jianxin, Yang Jingsui, et al.Geochemistry of high-grade metamorphic rocks of the North Qaidam mountains and their geological significance[J]. Journal of Asian Earth Sciences,2006,28:174-184.
[50] Luo Mingfei.Research on Early Palaeozoic Tectonic Characters of DHNS, GS[D].Chengdu: Chengdu University of Technology, 2010.
[罗明非. 甘肃党河南山早古生代大地构造性质研究[D].成都:成都理工大学,2010.]
[51] Lu S N, Yang C L, Li H K, et al.A group of rifting events in the terminal Paleoproterozoic in the North China Craton[J].Gondwana Research, 2002, 5: 123-131.
[52] Wu Huaichun, Zhang Shihong, Li Zhengxiang, et al.New paleomagnetic results from the Yangzhuang Formation of the Jixian System, North China, and tectonic implications[J]. Chinese Science Bulletin, 2005, 50(14): 1 483-1 489.
[53] Xia Linqi, Xia Zuchun, Xu Xueyi.Lithiogenesis of Marine Volcanic Rocks from North Qilian Mountains[M].Beijing: Geological Publish House, 1996.
[夏林圻,夏祖春,徐学义.北祁连山海相火山岩岩石成因[M].北京:地质出版社,1996.]
[54] Xia Linqi, Xia Zuchun, Xu Xueyi.Early Palaeozoic Mid-ocean Ridge-ocean Island and Back-arc basin volcanism in the north Qilian Mountains[J]. Acta Geologica Sinica, 1998,72(4):301-312.
[夏林圻,夏祖春,徐学义.北祁连山早古生代洋脊—洋岛和弧后盆地火山作用[J].地质学报,1998,72(4):301-312.]
[13] [张旗, 孙晓猛, 周德进, 等. 北祁连蛇绿岩的特征, 形成环境及其构造意义[J]. 地球科学进展, 1997, 12(4):366-393.]
[14] Song Shuguang.Tectonic evolution of subductive complex belts in the North Qilian Mountains[J]. Advances in Earth Science, 1997, 12(4):351-365.
[宋述光. 北祁连山俯冲杂岩带的构造演化[J].地球科学进展,1997, 12(4):351-365.]
[15] Song Shuguang, Zhang Lifei, Niu Y, et al. Zircon U-Pb SHRIMP ages of eclogites from the North Qilian Mountains in NW China and their tectonic implication[J]. Chinese Science Bulletin, 2004,49(6):592-595.
[宋述光,张立飞,Niu Y,等.北祁连山榴辉岩SHRIMP定年及其构造意义[J].科学通报,2004,49(6):592-595.]
[16] Song Shuguang.High-pressure metamorphic rocks in the North Qilian oceanic subduction zone, China:A review[J].Geological Bulletin of China, 2009, 28(12):1 769-1 778.
[宋述光. 北祁连山古大洋俯冲带高压变质岩研究评述[J].地质通报,2009, 28(12):1 769-1 778.]
[17] Xia Xiaohong, Song Shuguang.Forming age and tectono-petrogenises of the Jiugequan ophiolite in the North Qilian Mountain, NW China[J]. Chinese Science Bulletin, 2010, 15(15):1 465-1 473.
[夏小洪, 宋述光.北祁连山肃南九个泉蛇绿岩形成年龄和构造环境[J]. 科学通报,2010, 15(15):1 465-1 473.]
[18] Wu Cailai, Xu Xueyi,Gao Qianming, et al.Early Palaezoic granitoid magmatism and tectonic in North Qilian,NW China[J]. Acta Petrologica Sinica,2010,26(4):1 027-1 044.
[吴才来,徐学义,高前明,等.北祁连早古生代花岗质岩浆作用及构造演化[J].岩石学报, 2010,26(4):1 027-1 044.]
[19] Wu Cailai, Yang Jingsui, Yang Hongyi, et al.Dating of two types of granite from north Qilian, China[J]. Acta Petrologica Sinica, 2004, 20(3): 425-432.
[吴才来,杨经绥,杨宏仪,等.北祁连东部两类I型花岗岩定年及其地质意义[J].岩石学报,2004,20(3):425-432.]
[20] Zhang Qi, Chen Yu, Zhou Dejin, et al.Geochemical characteristics and genesis of Dachadaban ophiolite in North Qilian area[J]. Science in China (Series D),1998,41(3): 277-281.
[21] Xia L Q, Xia Z C, Xu X Y.Magmagenesis in the Ordovician backarc basins of the Northern Qilian Mountains, China[J]. Geological Society of America Bulletin,203,115(12): 1 510-1 522.
[22] Tseng Chien-Yuan, Yang Huai-Jen, Yang Houng-Yi, et al.Continuity of the North Qilian and North Qinling orogenic belts, Central Orogenic System of China: Evidence from newly discovered Paleozoic adakitic rocks[J]. Gondwana Research, 2009,16(2): 285-293.
[23] Wu Cailai, Gao Yuanhong, Ronald Frost B, et al.An early Palaeozoic double-subduction model for the North Qilian oceanic plate: Evidence from zircon SHRIMP dating of granites[J]. International Geology Review,2011, 53(2): 157-181.
[24] Hou Qingye, Zhao Zhidan, Zhang Hongfei, et al.Indian Ocean-MORB-type isotopic signature of Yushigou ophiolite in North Qilian Mountains and its implications[J]. Science in China (Series D),2006,49(6): 561-572.
[25] Smith A D, Yang H Y.The neodymium isotopic and geochemical composition of serpentinites from ophiolitic assemblages in the Qilian fold belt, northwest China[J]. Journal of Asian Earth Sciences, 2006,28(2): 119-132.
[26] Qiu Jiaxiang, Zeng Guangce, Zhu Yunhai. Characteristics and latitudinal comparative research on the early palaeozoic volcanic rocks of riftedorogenic belt and small ocean basinophiolite suit from northern Qinling Mountains and southern Qilian Mountains[J].Geological Journal of China Universities,1998,4(4):393-405.
[邱家骧,曾广策,朱云海,等.北秦岭—南祁连早古生代裂谷造山带火山岩与小洋盆蛇绿岩套特征及纬向对比[J].高校地质学报,1998,4(4):393-405.]
[27] Zhang Wangsheng, Feng Guangsheng, Gao Shan, et al.Metamorphic core complex structure and uplifting mechanism in Lajishan-Hualong area[J].Earth Science—Journal of China University of Geosciences, 2003,28(4):407-413.
[张旺生,冯光胜,高山,等.拉脊山—化隆变质核杂岩构造及其隆升机制探讨[J].地球科学——中国地质大学学报,2003,28(4):407-413.]
[28] Zhang Zhaowei, Li Wenyuan, Gao Yongbao, et al.ID-TIMS zircon U-Pb age of Yulonggou intrusive rocks in Southern Qilian Mountains and its geological significance[J]. Geological Bulletin of China, 2012, 31(2/3): 455-462.
[55] Zhang Jianxin, Xu Zhiqin, Chen Wen, et al.A Tentative discussion on the ages of the subduction-accretionary complex/ volcanic arcs in the middle sector of North Qilian Mountain[J]. Acta Petrologica et Mineralogica, 1997,16:112-119.
[张建新,许志琴,陈文,等.北祁连中段俯冲—增生杂岩/火山弧的时代探讨[J].岩石矿物杂志,1997,16:112-119.]
[56] Zhang Jianxin, Xu Zhiqin, Xu Huifen, et al.Framework of north Qilian Caledonian subduction-accretionary wedge and its deformation dynamics[J]. Scientia Geologica Sinica, 1998,33:290-299.
[张建新,许志琴,徐惠芬,等.北祁连加里东期俯冲—增生楔结构及动力学[J].地质科学,1998,33:290-299.]
[57] Wang Quan, Liu Xueya.The Caledonia Period Multicycle Paired Metamorphic Belts of Qilian[M]. Beijing: Geological Publish House, 1981.
[王荃,刘雪亚.祁连加里东期多旋回双变质带[M].北京:地质出版社,1981.]
[58] Liu Chuanzhou, Xiao Wenjiao, Yuan Chao, et al.The petrological and geochemical characteristics of the Zhamashi complex, Qilian Mountain and their tectonic implications[J]. Acta Petrologica Sinica, 2005,21(1):57-64.
[刘传周,肖文交,袁超,等.祁连山扎麻什基性杂岩体岩石地球化学特征及其大地构造意义[J].岩石学报,2005,21(1):57-64.]
[59] Zuo Guochao, Wu Hanquan.A bisubduction-collision orogenic model of early-paleozoic in the middle part of North Qilian area[J]. Advances in Earth Science, 1997,12(4):315-312.
[左国朝,吴汉泉.北祁连中段早古生代双向俯冲—碰撞造山模式剖析[J].地球科学进展, 1997,12(4):315-312.]
[60] Wu Cailai, Yao Shangzhi, Yang Jingsui, et al.Double subduction of the Early Paleozoic North Qilian oceanic plate: Evidence from granites in the central segment of North Qilian, NW China[J]. Geology in China, 2006,33(6):1 198-1 208.
[28] [张照伟,李文渊,高永宝,等.南祁连裕龙沟岩体ID-TIMS锆石U-Pb年龄及其地质意义[J].地质通报,2012,31(2/3):455-462.]
[29] Liu Zhiwu, Wang Chongli, Shi Xiaohu.Granitoids characteristics and tectonic setting of Danghenanshan area in South Qilian Mountains[J].Geoscience, 2006,20(4):545-554.
[刘志武,王崇礼,石小虎.南祁连党河南山花岗岩类特征及其构造环境[J].现代地质,2006,20(4):545-554.]
[30] Liu Zhiwu, Wang Chongli.Granitoid geochemistry and gold-copper mineralization in the Danghenanshan area,Southern Qilian Mountains[J]. Geology and Prospecting, 2007, 43(1): 64-73.
[刘志武, 王崇礼. 南祁连党河南山花岗岩类地球化学及其金铜矿化[J]. 地质与勘探, 2007, 43(1): 64-73.]
[31] Yong Yong,Xiao Wenjiao, Yuan Chao,et al.Geochronology and geochemistry of Paleozoic granitic plutons from the eastern Central Qilian and their tectonic implications[J].Acta Petrologica Sinica, 2008, 24(4): 855-866.
[雍拥,肖文交,袁超,等.中祁连东段古生代花岗岩的年代学、地球化学特征及其大地构造意义[J].岩石学报,2008, 24(4): 855-866.]
[32] Chen Junlu, Xu Xueyi, Zeng Zuoxun, et al.Geochemical characters and LA-ICPMS zircon U-Pb dating constraints on the petrogenesis and tectonic setting of the Shichuan intrusion, east segment of the Central Qilian, NW China[J]. Acta Petrologica Sinica, 2008,24(4):841-854.
[陈隽璐,徐学义,曾佐勋,等.中祁连东段什川杂岩基的岩石化学特征及年代学研究[J].岩石学报,2008,24(4):841-854.
[33] Guo Jinjing, Zhao Fengqing, Li Huaikun.Jinningian Col lisional Granite Belt in the Eastern Sector of the Central Qilian massif and its implication[J].Acta Geoscientia Sinica,1999,20(1):10-15.
[郭进京,赵凤青,李怀坤.中祁连东段晋宁期碰撞型花岗岩及其地质意义[J].地球学报,1999,20(1):10-15.]
[60] [吴才来,姚尚志,杨经绥,等.北祁连洋早古生代双向俯冲的花岗岩证据[J].中国地质,2006,33(6):1 198-1 208.]
[61] Wang Yonghe, Jiao Yangquan, Li Jianxing, et al. Ordovician magmatic arc stratum of the Middle Qilian Block[J]. Geoscience, 2008,22(5):724-732.
[王永和,焦养泉,李建星,等.中祁连北缘奥陶纪岩浆弧地层[J].现代地质,2008,22(5):724-732.]
[62] Qi Ruirong.LA-ICP-MS Zircon U-Pb ages and geological implications for the Bagadeerji Granitic plutons in the central Qilian Mountains, Gansu[J]. Sedimentary Geology and Tethyan Geology, 2012,32(4):86-93.
[齐瑞荣. 中祁连西段巴嘎德尔基岩体 LA-ICP-MS锆石U-Pb年龄及地质意义[J].沉积与特提斯地质,2012,32(4):86-93.]
[63] Wang Honghao,Li Jianghai,Yang Jingyi, et al.Paleo-plate Reconstruction and Drift Path of Tarim Block from Neoproterozic to Early Palaeozoic[J].Advances in Earth Science, 2013,28(6):637-647.
[王洪浩,李江海,杨静懿,等.塔里木陆块新元古代—早古生代古板块再造及漂移轨迹[J].地球科学进展,2013,28(6):637-647.]
[64] Compston W, Williams I S, Kirschvink J L, et al.Zircon U-Pb ages for the Early Cambrian time-scale[J]. Journal of Geological Society of London, 1992,149:171-184.
[65] Song Biao, Zhang Yumei, Wan Yusheng, et al.Mount making and procedure of the SHRIMP dating[J]. Geological Review,2002,48(Suppl.):26-30.
[宋彪,张玉梅,万渝生,等.锆石SHRIMP样品靶制作、年龄测定及有关现象讨论[J].地质论评,2002,48(增刊):26-30.]
[66] Govindaraju G.Compilation of working values and sample description for 383 geostandards[J]. Geostandards Newsletter, 1994,18: 1-158.
[67] Li X H.Geochemistry of the Longsheng ophiolite from the southern margin of Yangtze craton, SE China[J]. Geochemical Journal, 1997,31: 323-327.
[68] Liu Ye, Liu Xiaoming, Hu Zhaochu, et al.Evaluation of accuracy and long-term stability of determination of 37 trace elements in geological samples by ICP-MS[J]. Acta Petrologica Sinica, 2007,23(5):1 203-1 210.
[刘晔,柳小明,胡兆初,等. ICP-MS测定地质样品中37个元素的准确度和长期稳定性分析[J].岩石学报,2007,23(5):1 203-1 210.]
[69] Pidgeon R T, Nemchin A A, Hitchen G J.Internal strctures of zircons from Archaean granites from the Darling Range batholith: Implications for zircon stability and the interpretation of zircon U-Pb ages[J]. Contribution to Mineralogy Petrology, 1998,132:288-299.
[70] Le Maitre R W, Streckeisen A, Zanettin B, et al. A Classification of Igneous Rock Sand Glossary of Terms[M]. Oxford: Blackwell, 1989.
[71] Rickwood P C.Boundary lines within petrologic diagrams which use oxides of major and minor elements[J]. Lithos, 1989,22(4):247-263.
[72] Maniar P D, Piccoli P M.Tectonic discrimination of granitoids[J]. Geological Society of America Bulletin, 1989,101(5): 635-643.
[73] Sun S S, McDonough W F. Chemical and isotopic systematics of oceanic basalts: Implications for mantle composition and processes[J]. Geological Society, London, Special Publications, 1989,42(1): 313-345.
[74] Harris N B W, Pearce J A, Tindle A G. Geochemical characteristics of collision-zone magmatism[J]. Geological Society, London, Special Publications, 1986,19(1):67-81.
[75] Castillo Paterno R.An overview of adakite petrogenesis[J]. Chinese Science Bulletin, 2006,51(3):257-268.
[76] Rapp R P, Shimuzu N.Arc-magmatism in hot subduction zones: Interactions between slab-derived melts and the mantle wedge and the petrogenesis of adakites and high magnesium andesites (HMA)[C]∥Journal of Physics: Conference Series,1996,1: 497.
[77] Defant M J, Drummond M S.Derivation of some modern arc magmas by melting of Young subducted lithosphere[J].Nature, 1990,347: 662-665.
[78] Defant M J, Drummond M S. Mount St.Heles: Potential example of the partial melting of the subducted Lithosphere in a volcanic arc[J]. Geology, 1993,21:547-550.
[79] Kay S M, Romas V A, Marquez M.Evidence in Cerro pampa volcanic rocks for slab-melting prior to ridge-trench collision in southern South America[J]. The Journal of Geology,1993, 101:703-714.
[80] Martin H.Adakitic magmas: Modern analogues of Archaean granitoids[J]. Lithos, 1999,46:411-429.
[81] Drummond M S, Defant M J.A model for Trondhjemite-Tonalite-Dacite Genesis and Crustal Growth Via Slab Melting: Archean to Modern Comparisons[J]. Journal of Geophysical Research: Solid Earth, 1990,95(B13): 21 503-21 521.
[82] Peccerillo A, Taylor S R.Geochemistry of eocene Calc-Alkaline volcanic rocks from the Kastamonu area, Northern Turkey[J]. Contributions to Mineralogy and Petrology, 1976, 58(1): 63-81.
[83] Zhang Qi, Wang Yan, Qian Qing, et al.The characteristics and tectonic-metallogenic significances of the adakites in Yanshan period from eastern China[J]. Acta Petrologica Sinica, 2001,17(2):236-244.
[张旗, 王焰, 钱青,等.中国东部燕山期埃达克岩特征及其构造—成矿意义[J]. 岩石学报, 2001,17(2):236-244.]
[84] Zhang Qi, Qian Qing, Wang Erqi, et al.An east China plateau in mid-late Yanshanian period: Implication fromadakites[J]. Chinese Journal of Geology, 2001,36(2):248-255.
[张旗, 钱青,王二七,等.燕山中晚期的中国东部高原:埃达克岩的启示[J].地质科学,2001,36(2):248-255.]
[34] Guo Jinjing, Zhao Fengqing, Li Huaikun,et al.New chronological evidence of the age of Huangyuan Group in the eastern segment of Mid-Qilian massif and its geological significance[J].Regional Geology of China, 2000,19(1):26-31.
[郭进京,赵凤青,李怀坤,等.中祁连东段湟源群的年代学新证据及其地质意义[J].中国区域地质,2000,19(1):26-31.]
[35] He Shiping,Wang Honglung, Chen Juanlu,et al.LA-ICP-MS U-Pb zircon geochronology of basic dikes within Maxianshan Rock Group in the Central Qilian Mountains and its tectonic implications[J]. Earth Science, 2008,33(1):35-45.
[何世平,王洪亮,陈隽璐,等.中祁连马衔山岩群内基性岩墙群锆石LA-ICP-MS U-Pb年代学及其构造意义[J].地球科学,2008,33(1):35-45.]
[36] Yan Haiqing, Qian Zhuangzhi, Liu Jiqing, et al.New evidences of Micropaleoplants for the time of the Gaolan rock Group in the eastern section of the central Qilian Mountains[J]. Geological Review, 2005,51(2): 113-119.
[闫海卿,钱壮志,刘继庆,等.中祁连山东段皋兰岩群地质时代的微古植物新证据[J].地质论评, 2005,51(2): 113-119.]
[85] Zhang Qi, Wang Yan, Wang Yuanlong.Preliminary study on the components of the lower crust in east China Plateau during Yanshanian period: Constraints on Sr and Nd isotopic composltions of adakite-like rocks[J]. Acta Petrologica Sinica, 2001,17(4):505-513.
[张旗, 王焰, 王元龙.燕山期中国东部高原下地壳组成初探:埃达克质岩Sr、Nd同位素制约[J]. 岩石学报,2001,17(4):505-513.]
[86] Xia Linqi, Xia Zuchun, Xu Xueyi.Dynamics of Tectono-volcano-magmatic evolution from North Qilian Mountains, China[J]. Northwest Geoscience, 1995,(1):1-28.
[夏林圻,夏祖春,徐学义.北祁连山构造—火山岩浆演化动力学[J]. 西北地质科学,1995,(1): 1-28.]
[87] Hou Qingye, Zhao Zhidan, Zhang Hongfei, et al.Indian Ocean-MORB-type isotopic signature of Yushigou ophiolite in North Qilian Mountains and its implications[J]. Science in China(Series D),2005,35(8):710-719.
[侯青叶,赵志丹,张宏飞,等.北祁连玉石沟蛇绿岩印度洋MORB型同位素组成特征及其地质意义[J].中国科学:D辑,2005,35(8):710-719.]
[88] Song Shuguang, Zhang Guibin, Zhang Cong, et al.Dynamic process of oceanic subduction and continental collision: Petrological constraints of HP-UHP belts in Qilian-Qaidam, the northern Tibetan Plateau[J]. Chinese Science Bulletin, 2013, 58: 2 240-2 245.
[宋述光, 张贵宾, 张聪, 等. 大洋俯冲和大陆碰撞的动力学过程: 北祁连—柴北缘高压—超高压变质带的岩石学制约[J]. 科学通报, 2013, 58: 2 240-2 245.]
[1] 张瑞刚, 高雪, 杨立强. 岩浆混合作用的识别:以义敦岛弧稻城岩体为例[J]. 地球科学进展, 2018, 33(10): 1058-1074.
[2] 王晓先, 张进江, 王佳敏. 喜马拉雅早古生代岩浆事件:以吉隆和聂拉木眼球状片麻岩为例[J]. 地球科学进展, 2016, 31(4): 391-402.
[3] 杨婧, 王金荣, 张旗, 陈万峰, 潘振杰, 焦守涛, 王淑华. 弧后盆地玄武岩(BABB)数据挖掘:与MORB及IAB的对比[J]. 地球科学进展, 2016, 31(1): 66-77.
[4] 方维萱, 李建旭. 智利铁氧化物铜金型矿床成矿规律、控制因素与成矿演化[J]. 地球科学进展, 2014, 29(9): 1011-1024.
[5] 姚素平,丁 海,胡凯,焦堃. 我国南方早古生代聚煤过程中硫的生物地球化学行为及成矿效应[J]. 地球科学进展, 2010, 25(2): 174-183.
[6] 杨永亮. 10 Be在大洋边缘海洋学中的应用及模型[J]. 地球科学进展, 2002, 17(3): 355-362.
[7] 王强,许继锋,赵振华. 一种新的火成岩——埃达克岩的研究综述[J]. 地球科学进展, 2001, 16(2): 201-208.
[8] 张魁武,张旗,李达周. 阿拉斯加里镁铁—超镁铁杂岩的研究历史和现状[J]. 地球科学进展, 1990, 5(6): 48-51.
阅读次数
全文


摘要

版权所有 © 《地球科学进展》编辑部
地址：甘肃省兰州市天水中路8号
QQ：114723517
电话：0931-8762293　E-mail：adearth@lzb.ac.cn
陇ICP备2021001824号-5　 甘公网安备62010202000687