Zircon U-Pb age and Hf isotopes of the biotite plagioclase genesis in Duobagou area, Gansu Province
-
摘要:
通过对多坝沟地区敦煌杂岩中黑云斜长片麻岩LA-ICP-MS锆石U-Pb年龄和Lu-Hf同位素的研究，对敦煌杂岩的形成时代和敦煌地块的前寒武纪地壳生长演化进行探讨。锆石U-Pb年代学研究表明，710Ma代表了敦煌杂岩的最大沉积时代，黑云斜长片麻岩发育422Ma的早古生代变质事件，表明敦煌地块卷入了早古生代古亚洲洋俯冲-碰撞的演化过程。锆石Hf同位素研究结果表明，敦煌地块具有幕式生长特征，经历了约2.7Ga、2.5Ga、2.3Ga、2.0Ga和1.8Ga多个地壳生长时期。黑云斜长片麻岩发育的约0.9Ga和约0.8Ga的峰值年龄表明，敦煌地块新元古代构造热事件可与塔里木克拉通对比。
-
关键词:
- 多坝沟 /
- 敦煌杂岩 /
- 碎屑锆石U-Pb年龄 /
- 锆石Lu-Hf同位素
Abstract:The LA-ICP-MS zircon U-Pb age and zircon Lu-Hf isotope were analyzed for biotite-plagioclase gneiss from Duoba-gou area, Dunhuang terrain, with the purpose of determining the formation age of the Dunhuang complex and discussing the crustal growth and evolution history of the Dunhuang terrain during Precambrian. Zircon U-Pb dating results indicate that the maximum depositional age of supracrustal rocks from the Dunhuang complex is ca. 710Ma. Additionally, the studied biotite-plagioclase gneiss indicates a metamorphic event at 422Ma, suggesting that the Precambrian Dunhuang terrain might have been involved in the subduc-tion-collision process of the Paleo-Asian Ocean during Early Paleozoic. Zircon Hf isotopes show that the Dunhuang terrain experi-enced episodic crustal growth events at ca. 2.7Ga, ca.2.5Ga, ca. 2.3Ga, ca. 2.0Ga and ca. 1.8Ga, suggesting episodic crustal growth. It is considered that the tectonic attribute could be compared with that of the Tarim craton during Neoproterozoic, as shown by the peak age at ca. 0.9Ga and ca. 0.8Ga.
-
Keywords:
- Duobagou area /
- Dunhuang complex /
- detrital zircon U-Pb age /
- zircon Lu-Hf isotope
-
致谢: 样品测试过程中得到了西北大学大陆动力国家重点实验室第五春荣、戴梦宁、张红等老师的大力帮助，成文过程得到中国地质调查局西安地质调查中心孙吉明、李平工程师的帮助，在此一并表示感谢。
-
![]()
![]()
图 2 多坝沟黑云斜长片麻岩特征
Bt—黑云母；Qtz—石英；Pl—斜长石
Figure 2. Characteristics of biotite-plagioclase gneiss from Duobagou
![]()
图 4 敦煌杂岩锆石U-Pb年龄谐和图和年龄频谱图
Figure 4. U-Pb concordia diagrams, histograms and relative probability plots of zircons from Dunhuang complex
表 1 黑云斜长片麻岩LA-ICP-MS锆石U-Th-Pb同位素测试数据
Table 1 LA-ICP-MS zircon U-Th-Pb analytical data of biotite-plagioclase gneiss
测点号 比值 年龄/Ma 含量/10-6 Th/U Pb207/Pb206 1σ Pb207/U235 1σ Pb206/U238 1σ Pb208/Th232 1σ Pb207/Pb206 1σ Pb206/U238 1σ Pb208/Th232 1σ Th232 U238 09-4-2-01 0.12465 0.00287 6.44475 0.10097 0.37491 0.00451 0.10784 0.00134 2023.8 40.21 2052.5 21.15 2070 24.43 196.01 557.65 0.35 09-4-2-02 0.12510 0.00302 6.55485 0.11238 0.37994 0.00468 0.10511 0.00146 2030.2 42.12 2076 21.88 2020.2 26.73 115.56 173.71 0.67 09-4-2-03 0.13556 0.00297 6.44071 0.09108 0.34453 0.00406 0.10425 0.00111 2171.2 37.7 1908.4 19.47 2004.4 20.32 302.31 760 0.40 09-4-2-04 0.12888 0.00294 6.43490 0.09880 0.36206 0.00434 0.11058 0.00137 2082.7 39.56 1991.9 20.55 2119.9 25 146.92 248.15 0.59 09-4-2-05 0.13361 0.00302 6.50991 0.09813 0.35330 0.00422 0.10191 0.00113 2146 38.94 1950.3 20.13 1961.5 20.82 118.13 391.93 0.30 09-4-2-06 0.13518 0.00292 6.60636 0.09077 0.35438 0.00415 0.10921 0.00111 2166.3 37.23 1955.5 19.75 2094.9 20.3 301.35 387.01 0.78 09-4-2-07 0.12596 0.00363 6.35668 0.14491 0.36595 0.00498 0.09875 0.00166 2042.3 50.1 2010.3 23.5 1903.5 30.59 232.47 340.95 0.68 09-4-2-08 0.12922 0.00309 6.72697 0.11323 0.37750 0.00464 0.10843 0.00138 2087.3 41.45 2064.6 21.72 2080.8 25.23 138.15 226.73 0.61 09-4-2-09 0.08332 0.00200 2.44812 0.04179 0.21305 0.00254 0.06420 0.00070 1276.6 46.21 1245 13.52 1257.6 13.22 323.92 453.84 0.71 09-4-2-10 0.12580 0.00341 6.50252 0.13519 0.37481 0.00492 0.11080 0.00189 2040.1 47.16 2052 23.07 2124 34.46 89.48 158.91 0.56 09-4-2-11 0.12920 0.00325 6.69396 0.12318 0.37570 0.00474 0.11417 0.00160 2087.1 43.57 2056.2 22.23 2185.2 29.05 147.77 255.17 0.58 09-4-2-12 0.12643 0.00282 6.51552 0.09564 0.37370 0.00443 0.11067 0.00128 2048.9 38.85 2046.8 20.79 2121.6 23.26 126.56 201.54 0.63 09-4-2-13 0.20171 0.00438 10.27964 0.14133 0.36954 0.00440 0.11636 0.00254 2840.1 34.95 2027.2 20.71 2224.8 46.01 45.12 454.94 0.10 09-4-2-14 0.07727 0.00176 1.52452 0.02357 0.14306 0.00167 0.04820 0.00074 1128.2 44.75 862 9.44 951.5 14.27 158.65 1104.93 0.14 09-4-2-15 0.05722 0.00209 0.55137 0.01757 0.06987 0.00094 0.02201 0.00052 499.6 79.07 435.4 5.65 440 10.22 119.6 354.49 0.34 09-4-2-16 0.05687 0.00214 0.54224 0.01792 0.06914 0.00094 0.02127 0.00055 485.8 81.67 431 5.66 425.4 10.9 86.81 308.82 0.28 09-4-2-17 0.25464 0.00527 17.12490 0.21077 0.48766 0.00566 0.15081 0.00187 3213.8 32.31 2560.6 24.52 2839.2 32.81 157.35 373.17 0.42 09-4-2-18 0.05790 0.00226 0.53224 0.01842 0.06666 0.00092 0.02136 0.00056 525.5 83.8 416 5.58 427.2 11.11 113.7 382.78 0.30 09-4-2-19 0.05649 0.00378 0.50964 0.03217 0.06542 0.00123 0.02058 0.00106 470.9 142.19 408.5 7.42 411.7 21.04 101.74 374.03 0.27 09-4-2-20 0.05744 0.00304 0.51209 0.02509 0.06464 0.00105 0.02019 0.00073 508.1 112.69 403.8 6.33 404 14.41 162.59 164.83 0.99 09-4-2-21 0.07241 0.00190 1.63795 0.03280 0.16404 0.00200 0.05008 0.00071 997.4 52.52 979.2 11.09 987.7 13.75 191.88 513.46 0.37 09-4-2-22 0.16479 0.00533 8.68040 0.22990 0.38197 0.00589 0.11132 0.00278 2505.4 53.43 2085.5 27.45 2133.3 50.53 57.45 97.47 0.59 09-4-2-23 0.05531 0.00159 0.52478 0.01210 0.06880 0.00084 0.02124 0.00032 425.1 62.03 428.9 5.09 424.7 6.28 404 872.55 0.46 09-4-2-24 0.05593 0.00287 0.53808 0.02548 0.06976 0.00110 0.02826 0.00135 449.1 110.31 434.7 6.61 563.3 26.6 27.63 103.49 0.27 09-4-2-25 0.07350 0.00364 1.38773 0.06288 0.13692 0.00228 0.03863 0.00070 1027.7 97.1 827.2 12.94 766.2 13.61 77.69 299.14 0.26 09-4-2-26 0.05585 0.00224 0.51034 0.01822 0.06626 0.00092 0.02070 0.00056 446.2 86.57 413.6 5.57 414 11.05 78.39 280.64 0.28 09-4-2-27 0.05516 0.00302 0.50563 0.02576 0.06647 0.00109 0.01956 0.00073 418.6 117.43 414.9 6.57 391.6 14.53 141.06 410.06 0.34 09-4-2-28 0.05489 0.00212 0.49710 0.01698 0.06567 0.00090 0.01971 0.00048 407.8 83.68 410 5.42 394.6 9.46 79.96 281.43 0.28 09-4-2-29 0.14240 0.00854 4.30952 0.23508 0.21945 0.00524 0.07573 0.00452 2256.6 100.04 1279 27.68 1475.4 85.02 17.74 42.16 0.42 09-4-2-30 0.16591 0.00374 10.79940 0.16162 0.47200 0.00572 0.13195 0.00163 2516.8 37.39 2492.3 25.04 2505.1 29.11 285.08 405.2 0.70 09-4-2-31 0.06616 0.00311 1.29303 0.05542 0.14172 0.00223 0.04206 0.00072 811.4 95.41 854.4 12.58 832.7 13.99 136.64 91.46 1.49 09-4-2-32 0.11213 0.00318 5.05660 0.11295 0.32700 0.00433 0.09068 0.00172 1834.2 50.55 1823.8 21.04 1754.5 31.93 54.66 126.02 0.43 09-4-2-33 0.11297 0.00273 4.90466 0.08443 0.31481 0.00385 0.08943 0.00129 1847.8 43.1 1764.3 18.87 1731.3 23.91 84.77 180.83 0.47 09-4-2-34 0.07366 0.00293 1.63652 0.05744 0.16109 0.00236 0.04700 0.00117 1032.3 78.27 962.8 13.12 928.2 22.62 71 458.01 0.16 09-4-2-35 0.07691 0.00329 1.70977 0.06535 0.16121 0.00249 0.05027 0.00143 1118.8 82.97 963.5 13.8 991.3 27.45 46.33 334.66 0.14 09-4-2-36 0.07016 0.00196 1.40141 0.03074 0.14483 0.00180 0.04318 0.00089 933.1 56.15 871.9 10.13 854.4 17.21 51.48 399.04 0.13 09-4-2-37 0.07353 0.00244 1.66026 0.04644 0.16372 0.00219 0.04839 0.00118 1028.7 65.6 977.4 12.15 955.1 22.8 67.39 199 0.34 09-4-2-38 0.06403 0.00263 1.02776 0.03774 0.11639 0.00168 0.03502 0.00062 742.6 84.68 709.8 9.71 695.8 12.05 173.51 248.47 0.70 09-4-2-39 0.18938 0.00468 11.77300 0.20784 0.45078 0.00586 0.12170 0.00177 2736.8 40.06 2398.7 26.02 2321.3 31.93 116.33 161.34 0.72 09-4-2-40 0.16436 0.00372 6.32886 0.09512 0.27922 0.00337 0.11537 0.00314 2501 37.59 1587.4 16.98 2207 56.99 30.5 370.41 0.08 09-4-2-41 0.07080 0.00237 1.63194 0.04619 0.16714 0.00224 0.04917 0.00063 951.7 66.91 996.3 12.35 970.1 12.22 219.91 164.03 1.34 09-4-2-42 0.07262 0.00200 1.69077 0.03644 0.16882 0.00210 0.04981 0.00080 1003.5 54.62 1005.6 11.56 982.4 15.34 186.45 354.5 0.53 09-4-2-43 0.07301 0.00244 1.69365 0.04790 0.16820 0.00226 0.04784 0.00130 1014.4 66.28 1002.2 12.48 944.5 25.11 199.98 352.58 0.57 09-4-2-44 0.05623 0.00204 0.53523 0.01687 0.06902 0.00092 0.02119 0.00048 460.8 78.5 430.2 5.55 423.8 9.55 139.37 446.68 0.31 09-4-2-45 0.18596 0.00646 12.98249 0.37670 0.50624 0.00858 0.13595 0.00432 2706.7 56.2 2640.6 36.74 2576.5 76.8 30.58 128.04 0.24 09-4-2-46 0.07034 0.00199 1.59914 0.03584 0.16485 0.00206 0.05183 0.00082 938.3 56.89 983.7 11.4 1021.4 15.83 138.34 399.99 0.35 09-4-2-47 0.17181 0.00376 9.84696 0.13856 0.41558 0.00495 0.11806 0.00154 2575.4 36.13 2240.4 22.53 2255.6 27.77 110.77 266.9 0.42 09-4-2-48 0.07006 0.00321 1.35679 0.05629 0.14043 0.00221 0.04589 0.00095 930 91.25 847.1 12.47 906.8 18.36 67.18 281.18 0.24 09-4-2-49 0.05846 0.00205 0.54689 0.01648 0.06783 0.00090 0.02923 0.00153 547.2 74.64 423.1 5.41 582.4 30.04 47.99 351.22 0.14 09-4-2-50 0.05538 0.00204 0.51995 0.01676 0.06808 0.00091 0.02045 0.00047 427.2 80.02 424.6 5.51 409.2 9.31 154.88 489.35 0.32 09-4-2-51 0.05631 0.00247 0.53689 0.02125 0.06913 0.00100 0.02107 0.00062 463.9 94.93 430.9 6.05 421.4 12.22 118.13 391.93 0.30 09-4-2-52 0.05514 0.00235 0.51106 0.01963 0.06721 0.00096 0.02013 0.00051 417.8 92.29 419.3 5.8 402.9 10.2 196.01 557.65 0.35 
下载: 导出CSV
表 2 黑云斜长片麻岩Hf同位素组成
Table 2 Analytical data of zircon Hf isotope composition of biotite-plagioclase gneiss
测点号 年龄/Ma 176Yb/177Hf 176Lu/177Hf 176Hf/177Hf (176Hf/177Hf)i 2σ εHf(0) εHf(t) TDM1 TDM2 fLu/Hf 09-4-2-2 2030 0.012233 0.000341 0.281447 0.281434 0.000036 -47.33 -2.50 2497 2786 -0.99 09-4-2-3 2171 0.014274 0.000390 0.281643 0.281627 0.000028 -40.51 7.48 2240 2283 -0.99 09-4-2-4 2083 0.012453 0.000354 0.281600 0.281586 0.000039 -41.94 4.08 2293 2423 -0.99 09-4-2-5 2166 0.022294 0.000602 0.281662 0.281638 0.000035 -40.12 7.44 2238 2281 -0.98 09-4-2-6 2042 0.020220 0.000554 0.281646 0.281625 0.000040 -40.57 4.27 2252 2380 -0.98 09-4-2-7 2087 0.014410 0.000406 0.281585 0.281569 0.000041 -42.55 3.49 2319 2462 -0.99 09-4-2-8 1277 0.034685 0.000918 0.282166 0.282144 0.000030 -22.21 5.31 1558 1725 -0.97 09-4-2-9 2040 0.009860 0.000279 0.281441 0.281430 0.000033 -47.45 -2.31 2498 2782 -0.99 09-4-2-10 2049 0.012387 0.000374 0.281429 0.281414 0.000041 -48.01 -2.81 2525 2820 -0.99 09-4-2-11 2087 0.011805 0.000335 0.281581 0.281568 0.000040 -42.58 3.56 2316 2458 -0.99 09-4-2-13 862 0.012118 0.000249 0.281981 0.281977 0.000028 -28.12 -9.26 1758 2317 -0.99 09-4-2-14 435 0.031385 0.000886 0.282506 0.282499 0.000030 -9.65 -0.34 1062 1435 -0.97 09-4-2-15 3214 0.024149 0.000684 0.280779 0.280737 0.000025 -71.96 -0.93 3455 3600 -0.98 09-4-2-17 416 0.035248 0.001013 0.282668 0.282660 0.000029 -3.96 4.91 838 1088 -0.97 09-4-2-19 409 0.027751 0.000770 0.282613 0.282607 0.000031 -5.82 2.96 907 1206 -0.98 09-4-2-20 404 0.020286 0.000545 0.282163 0.282158 0.000025 -21.70 -12.98 1523 2206 -0.98 09-4-2-21 979 0.038970 0.001027 0.282316 0.282297 0.000023 -16.79 4.18 1349 1567 -0.97 09-4-2-22 2505 0.002344 0.000049 0.281426 0.281424 0.000040 -47.68 8.44 2492 2483 -1.00 09-4-2-24 435 0.016689 0.000452 0.282220 0.282216 0.000034 -19.67 -10.24 1440 2058 -0.99 09-4-2-25 827 0.019086 0.000558 0.282165 0.282156 0.000048 -21.77 -3.83 1526 1952 -0.98 09-4-2-26 414 0.024436 0.000700 0.282478 0.282473 0.000035 -10.57 -1.67 1093 1503 -0.98 09-4-2-27 415 0.033856 0.000941 0.282725 0.282717 0.000031 -1.93 6.94 756 959 -0.97 09-4-2-28 2257 0.052166 0.001402 0.281675 0.281615 0.000031 -40.92 7.46 2316 2350 -0.96 09-4-2-29 410 0.021766 0.000584 0.282783 0.282779 0.000026 0.23 9.09 664 818 -0.98 09-4-2-30 2517 0.038110 0.001126 0.281479 0.281424 0.000034 -47.66 6.90 2561 2587 -0.97 09-4-2-31 854 0.013956 0.000382 0.282324 0.282318 0.000032 -16.07 2.57 1298 1572 -0.99 09-4-2-32 1834 0.010011 0.000271 0.281497 0.281488 0.000027 -45.41 -4.91 2420 2784 -0.99 09-4-2-33 1848 0.023634 0.000604 0.281847 0.281826 0.000025 -33.45 7.00 1981 2062 -0.98 09-4-2-34 963 0.030647 0.000863 0.282092 0.282076 0.000044 -24.60 -3.89 1649 2059 -0.97 09-4-2-35 964 0.028223 0.000813 0.282280 0.282265 0.000047 -17.93 2.85 1386 1638 -0.98 09-4-2-37 977 0.022406 0.000549 0.282342 0.282332 0.000028 -15.55 5.69 1283 1470 -0.98 09-4-2-38 872 0.011952 0.000337 0.282364 0.282358 0.000030 -14.63 4.43 1240 1469 -0.99 09-4-2-39 2737 0.015357 0.000416 0.281174 0.281152 0.000033 -57.30 3.44 2880 2968 -0.99 09-4-2-41 996 0.012917 0.000328 0.281822 0.281816 0.000032 -33.82 -12.05 1981 2591 -0.99 09-4-2-43 1014 0.055249 0.001306 0.282481 0.282456 0.000026 -11.17 10.38 1134 1204 -0.96 09-4-2-44 430 0.038066 0.001041 0.282825 0.282817 0.000031 1.58 10.75 618 728 -0.97 09-4-2-45 2707 0.019976 0.000546 0.281315 0.281287 0.000053 -52.51 7.33 2708 2708 -0.98 09-4-2-46 984 0.031931 0.000781 0.282362 0.282348 0.000026 -15.00 6.25 1269 1441 -0.98 09-4-2-50 2575 0.025940 0.000736 0.281294 0.281258 0.000027 -53.53 2.96 2760 2872 -0.98 09-4-2-51 847 0.020067 0.000562 0.282301 0.282292 0.000075 -16.96 1.42 1339 1639 -0.98 09-4-2-53 423 0.018808 0.000532 0.282543 0.282539 0.000034 -8.25 0.90 997 1347 -0.98 09-4-2-55 425 0.032210 0.000885 0.282700 0.282693 0.000032 -2.78 6.32 789 1006 -0.97 09-4-2-54 431 0.039267 0.001092 0.282782 0.282773 0.000033 0.04 9.22 680 827 -0.97
下载: 导出CSV
-
李锦轶.新疆东部新元古代晚期和古生代构造格局及其演变[J].地质论评, 2004, 50(3):304-322. http://d.wanfangdata.com.cn/Periodical_dzlp200403015.aspx 梅华林, 于海峰, 李铨, 等.甘肃敦煌-北山早前寒武纪岩石组合-构造初步框架[J].前寒武纪研究进展, 1997, 20(4):47-54. http://www.cnki.com.cn/Article/CJFDTotal-YSXB201305018.htm 梅华林, 于海峰, 陆松年, 等.甘肃敦煌太古宙英云闪长岩:单颗粒锆石U-Pb年龄和Nd同位素[J].前寒武纪研究进展, 1998, 21(2):41-45. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=qhwjyjjz199802006 张建新, 李怀坤, 孟繁聪, 等.塔里木盆地东南缘(阿尔金山)"变质基底"记录的多期构造热事件:锆石U-Pb年代学的制约[J].岩石学报, 2011, 27(1):23-46. http://www.doc88.com/p-901231908735.html 孟繁聪, 张建新, 相振群, 等.塔里木盆地东北缘敦煌群的形成和演化:锆石U-Pb年代学和Lu-Hf同位素证据[J].岩石学报, 2011, 27(1):59-76. http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20110104 甘肃省地质矿产局.甘肃省区域地质志[M].北京:地质出版社, 1989:1-692. 新疆维吾尔自治区地质矿产局.新疆维吾尔自治区区域地质志[M].北京:地质出版社, 1993:1-135. 许志琴, 杨经绥, 张建新, 等.阿尔金断裂两侧构造单元的对比及岩石圈剪切机制[J].地质学报, 1999, 73(3):193-205. http://www.oalib.com/paper/4897721 Lu S N, Li H K, Zhang C L, et al. Geological and geochronological evidence for the Precambrian evolution of the Tarim Craton and surrounding continental fragments[J]. Precambrian Research, 2008, 160:94-107. doi: 10.1016/j.precamres.2007.04.025
辛后田, 刘永顺, 罗照华, 等.塔里木盆地东南缘阿克塔什塔格地区新太古代陆壳增生:米兰岩群和TTG片麻岩的地球化学及年代学约束[J].地学前缘, 2013, 20(1):240-259. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201301020 王洪亮, 徐学义, 何世平, 等. 1:100万中国天山及邻区地质图[M].北京:地质出版社, 2007. 徐学义, 何世平, 王洪亮, 等.中国西北部地质概论——秦岭、祁连、天山地区[M].北京:科学出版社, 2008. Zhao G C, Cawood P A. Precambrian geology of China[J]. Precambrian Research, 2012, 222/223:13-54. doi: 10.1016/j.precamres.2012.09.017
Zong K Q, Zhang Z M, He Z Y, et al. Early Palaeozoic high-pressure granulites from the Dunhuang block, northeastern Tarim Craton:constraints on continental collision in the southern Central Asian Orogenic Belt[J]. Journal of Metamorphic Geology, 2012, 30:753-768. doi: 10.1111/jmg.2012.30.issue-8
Long X P, Yuan C, Sun M, et al. New geochemical and combined zircon U-Pb and Lu-Hf isotopic data oforthogneisses in the northern AltynTagh, northernmargin of the Tibetanplateau:Implication for Archean evolution of the Dunhuang Block andcrust formation in NW China[J]. Lithos, 2014, 200/201:418-431. doi: 10.1016/j.lithos.2014.05.008
He Z Y, Zhang Z M, Zong K Q, et al. Metamorphic p-T-t evolution of mafic HP granulites in the northeastern segment of the Tarim Craton (Dunhuang block):Evidence for early Paleozoic continental subduction[J]. Lithos, 2014, 196/197:1-13. doi: 10.1016/j.lithos.2014.02.020
黄汲清, 任纪舜, 姜春发, 等.中国大地构造基本轮廓[J].地质学报, 1977, 2:117-135. https://www.wenkuxiazai.com/doc/679571ed5ef7ba0d4a733b0d.html 张振法, 李超英, 牛颖智.阿拉善敦煌陆块的性质、范围及其构造作用和意义[J].内蒙古地质, 1997, (2):1-14. https://www.wenkuxiazai.com/doc/464bb182bceb19e8b8f6baa7.html Zhang J X, Gong J H, Yu S Y. c. 1.85 Ga HP granulitefaciesmetamorphism in theDunhuang block of the TarimCraton, NW China:evidencefrom U-Pb zircon dating ofmafic granulites[J]. Journal of the Geological Society, 2012, 169:511-514. doi: 10.1144/0016-76492011-158
Zhang J X, Yu S Y, Gong J H, et al. The latest Neoarchean-Paleoproterozoic evolution of the Dunhuang block, eastern Tarim craton, northwestern China:Evidence from zircon U-Pb dating and Hf isotopic analyses[J]. Precambrian Research, 2013, 226:21-42. doi: 10.1016/j.precamres.2012.11.014
赵燕, 第五春荣, 孙勇, 等.甘肃敦煌水峡口地区前寒武纪岩石的锆石U-Pb年龄、Hf同位素组成及其地质意义[J].岩石学报, 2013, 29(5):1698-1712. http://www.ysxb.ac.cn/ysxb/ch/reader/create_pdf.aspx?file_no=20130517&journal_id=ysxb&year_id=2013 赵燕, 第五春荣, 朱涛, 等.敦煌三危山地区晚泥盆世斜长花岗岩的发现及其地质意义[J].岩石学报, 2015, 31(7):1855-1869. http://www.ysxb.ac.cn/ysxb/ch/reader/create_pdf.aspx?file_no=20150704&journal_id=ysxb&year_id=2015 Ge R F, Zhu W B, Wu H L, et al. Zircon U-Pb ages and Lu-Hf isotopes of Paleoproterozoic metasedimentary rocks in the Korla Complex, NW China:Implications for metamorphic zircon formation and geological evolution of the Tarim Craton[J]. Precambrian Research, 2013, 231:1-18. doi: 10.1016/j.precamres.2013.03.003
Wang Z M, Han C M, Xiao W J, et al. Petrology and geochronology of Paleoproterozoic garnet-bearing amphibolites from the Dunhuang Block, Eastern Tarim Craton[J]. Precambrian Research, 2014, 255:163-180. doi: 10.1016/j.precamres.2014.09.025
朱涛, 王洪亮, 徐学义, 等.敦煌地块南缘石炭纪埃达克岩的发现及其地质意义[J].岩石学报, 2014, 30(2):491-502. http://www.ysxb.ac.cn/ysxb/ch/reader/create_pdf.aspx?file_no=20140213&journal_id=ysxb&year_id=2014 王楠, 吴才来, 马昌前, 等.敦煌地块南部古生代花岗岩地球化学、锆石U-Pb定年及Hf同位素特征研究[J].岩石学报, 2016, 32(12):3753-3780. http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20161214 王楠, 吴才来, 马昌前, 等.敦煌地块三危山地区花岗岩体地球化学、锆石U-Pb及Hf同位素特征[J].地质学报, 2016, 90(10):2681-2705. doi: 10.3969/j.issn.0001-5717.2016.10.010 李荣社, 计文化, 潘晓平, 等. 1:100万昆仑山及邻区地质图[M].北京:地质出版社, 2008. 孙健初.祁连山一带地质史纲要[J].地质论评, 1942, 7(Z1):17-26. http://www.cnki.com.cn/Article/CJFDTOTAL-GSDZ198602004.htm 张志诚, 郭召杰, 邹冠群, 等.甘肃敦煌党河水库TTG地球化学特征、锆石SHRIMP U-Pb定年及其构造意义[J].岩石学报, 2009, 25(3):495-505. http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20090302 Zhao Y, Sun Y, Yan J H, et al. The Archean-Paleoproterozoic crustal evolution in the Dunhuangregion, NW China:Constraints from zircon U-Pb geochronology and in situ Hf isotopes[J]. Precambrian Research, 2015, 271:83-97. doi: 10.1016/j.precamres.2015.10.002
Zhao Y, Sun Y, Diwu C R, et al. The Dunhuang block is a Paleozoic orogenic belt and part of the Central Asian OrogenicBelt (CAOB), NW China[J]. Gondwana Research, 2016, 30:207-223. doi: 10.1016/j.gr.2015.08.012
Zhao Y, Sun Y, Diwu C R, et al. Paleozoic intrusive rocks from the Dunhuang tectonic belt, NW China:Constraints on the tectonic evolution of the southernmost Central Asian Orogenic Belt[J]. Journal of Asian Earth Sciences, 2017, 138:562-587. doi: 10.1016/j.jseaes.2017.02.037
Bao W H, Long X P, Yuan C, et al. Paleozoic adakitic rocks in the northern Altyn Tagh, northwest China:Evidence for progressive crustal thickening beneath the Dunhuang Block[J]. Lithos, 2017, 272/273:1-15. doi: 10.1016/j.lithos.2016.12.006
Wang Z M, Han C M, Xiao W J, et al. Paleoproterozoic subduction-related magmatism and crustal evolution of the Dunhuang Block, NW China[J]. Journal of Asian Earth Sciences, 2017, 134:13-28. doi: 10.1016/j.jseaes.2016.11.008
彭涛, 王浩, 陈泓旭, 等.甘肃敦煌观音沟地区变质作用初步研究[J].岩石学报, 2014, 30(2):503-511. http://www.ysxb.ac.cn/ysxb/ch/reader/create_pdf.aspx?file_no=20140214&journal_id=ysxb&year_id=2014 Wang H Y C, Wang J, Wang G D, et al. Metamorphic evolution and geochronology of the Dunhuang orogenic belt in the Hongliuxia area, northwestern China[J]. Journal of Asian Earth Sciences, 2017, 135:51-69. doi: 10.1016/j.jseaes.2016.12.014
Wang H Y C, Chen H X, Zhang Q, et al. Tectonic mélange records the Silurian-Devonian subduction Tectonic mélange records the Silurian-Devonian subduction southernmost Central Asian Orogenic Belt[J]. Geology, 2017, 45(5):427-430. doi: 10.1130/G38834.1
Yuan H L, Gao S, Liu X M, et al. Accurate U-Pb Age and Trace Element Determinations of Zircon by Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry[J]. Geostandards and Geoanalytical Research, 2004, 28(3):353-370. doi: 10.1111/ggr.2004.28.issue-3
Ludwig K R. Isoplot 3. 00: A Geochronological Toolkit for Micro-soft Excel[M]. Berkeley: Berkeley Geochronology Center, California, 2003.
Chu Nan-Chin, Taylor R N, Chavagnac V, et al. Hf isotope ratio analysis using multicollector inductively coupled plasma mass spectrometry:an evaluation of isobaric interference corrections[J]. Journal of Analytical Atomic Spectrometry, 2002, 17:1567-1574. doi: 10.1039/b206707b
Elhlou S, Belousova E, Griffin W L, et al. Trace element and isotopic composition of GJ-red zircon standard by laser ablation[C]//Goldschimidt Conference Abstracts, 2006, 70(Supp 1): A158.
Wu F Y, Yang Y H, Xie L W, et al. Hf isotopic compositions of the standard zircons and baddeleyites used in U-Pb geochronology[J]. Chemical Geology, 2006, 234:105-126. doi: 10.1016/j.chemgeo.2006.05.003
Blichert-Toft J, Albarede F. The Lu-Hf isotope geochemistry of chondrites and the evolution of the mantle-crust system[J]. Earth and Planetary Science Letter, 1997, 148:243-258. doi: 10.1016/S0012-821X(97)00040-X
Griffin W L, Pearson N J, Belousova E, et al. The Hf isotope composition of cratonic mantle LA-MC-ICP-MS analysis of zircon megacrysts in kimberlites[J]. Geochimica et Cosmochimica Acta, 2000, 64(1):133-147. doi: 10.1016/S0016-7037(99)00343-9
Amelin Y, Lee D C, Halliday A N. Early-middle Archaean crustal evolution deduced from Lu-Hf and U-Pb isotopic studies of sin-gle zircon grains[J]. Geochimica et Cosmochimica Acta, 2000, 64(24):4205-4225. doi: 10.1016/S0016-7037(00)00493-2
Condie K C, Aster R C. Episodic zircon age spectra of orogenic granitoids:The supercontinent connection and continental growth[J]. Precambrian Research, 2010, 180:227-236. doi: 10.1016/j.precamres.2010.03.008
Belousova E A, Griffin W L, O'Reilly S Y. Zircon crystal morphology, trace element signatures and Hf isotope composition as a tool for petrogenetic modelling:examples from eastern australian granitoids[J]. Journal of Petrology, 2006, 47(2):329-353. doi: 10.1093/petrology/egi077
Zong K Q, Liu Y S, Zhang Z M, et al. The generation and evolution of Archean continental crust in the Dunhuang block, north-eastern Tarim craton, northwestern China[J]. Precambrian Research, 2013, 235:251-263. doi: 10.1016/j.precamres.2013.07.002
王忠梅, 肖文交, 韩春明, 等.甘肃敦煌红柳峡地区石榴石斜长角闪岩的变质特征、锆石U-Pb年龄及地质意义[J].岩石学报, 2013, 29(5):1685-1697. http://www.cnki.com.cn/Article/CJFDTotal-YSXB201305018.htm Zhao G C, Wilde S A, Cawood P A, et al. Archean blocks and their boundaries in the North China Craton:lithological, geochemical, structural and P-T path constraints and tectonic evolution[J]. Precambrian Research, 2001, 107:45-73. doi: 10.1016/S0301-9268(00)00154-6
李三忠, 赵淑娟, 余珊, 等.东亚原特提斯洋(Ⅱ):早古生代微陆块亲缘性和聚合[J].岩石学报, 2016, 32(9):2628-2644. http://www.ysxb.ac.cn/ysxb/ch/reader/create_pdf.aspx?file_no=20160903&journal_id=ysxb&year_id=2016 Zhao G C, Guo J H. Precambrian geology of China:Preface[J]. Precambrian Research, 2012, 222/223:1-12. doi: 10.1016/j.precamres.2012.09.018
Liu Q, Zhao G C, Sun M, et al. Ages and tectonic implications of Neoproterozoic ortho-and paragneisses in the Beishan Orogenic Belt, China[J]. Precambrian Research, 2015, 266:551-578. doi: 10.1016/j.precamres.2015.05.022
姜洪颖, 贺振宇, 宗克清, 等.北山造山带南缘北山杂岩的锆石U-Pb定年和Hf同位素研究[J].岩石学报, 2013, 29(11):3949-3967. http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20131124 Yuan Y, Zong K Q, He Z Y, et al. Geochemical and geochrono-logical evidence for a former early Geochemical and geochronological evidence for a former early Geochemical and geochronological evidence for a former early[J]. Precambrian Research, 2015, 266:409-424. doi: 10.1016/j.precamres.2015.05.034
Zong K Q, Klemd R, Yuan Y, et al. The assembly of Rodinia:The correlation of early Neoproterozoic (ca. 900 Ma) high-grade metamorphism and continental arc formation in the southern Beishan Orogen, southern Central Asian Orogenic Belt (CAOB)[J]. Precambrian Research, 2017, 290:32-48. doi: 10.1016/j.precamres.2016.12.010
Zhang Z Y, Zhu W B, Shu L S, et al. Neoproterozoic ages of the Kuluketage diabase dyke swarm in Tarim, NW China, and its relationship to the breakup of Rodinia[J]. Geological Magazine, 2009, 146:150-154. doi: 10.1017/S0016756808005839
高林志, 王宗起, 许志琴, 等.塔里木盆地库鲁克塔格地区新元古代冰碛岩锆石SHRIMP U-Pb年龄新证据[J].地质通报, 2010, 29(2/3):205-213. http://dzhtb.cgs.cn/ch/reader/view_abstract.aspx?file_no=2010020304&flag=1 Long X P, Yuan C, Sun M, et al. Reworking of the Tarim Craton by underplating of mantle plume-derived magmas:Evidence from Neoproterozoic granitoids in the Kuluketage area, NW China[J]. Precambrian Research, 2011, 187:1-14. doi: 10.1016/j.precamres.2011.02.001
Zhang C L, Zou H B, Wang H Y, et al. Multiple phases of the NeoproterozoicigneousactivityinQuruqtaghofthenortheasternTarim Block, NW China:Interaction between plate subduction and mantle plume?[J]. Precambrian Research, 2012, 222/223:488-502. doi: 10.1016/j.precamres.2011.08.005
计量
- 文章访问数: 2496
- HTML全文浏览量: 312
- PDF下载量: 2855
