• 中国出版政府奖提名奖

    中国百强科技报刊

    湖北出版政府奖

    中国高校百佳科技期刊

    中国最美期刊

    留言板

    尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

    姓名
    邮箱
    手机号码
    标题
    留言内容
    验证码

    塔里木盆地巴楚地区上泥盆统-下石炭统沉积-物源记录及其构造演化

    郭春涛 高剑 李忠 张磊

    郭春涛, 高剑, 李忠, 张磊, 2017. 塔里木盆地巴楚地区上泥盆统-下石炭统沉积-物源记录及其构造演化. 地球科学, 42(3): 421-434. doi: 10.3799/dqkx.2017.032
    引用本文: 郭春涛, 高剑, 李忠, 张磊, 2017. 塔里木盆地巴楚地区上泥盆统-下石炭统沉积-物源记录及其构造演化. 地球科学, 42(3): 421-434. doi: 10.3799/dqkx.2017.032
    Guo Chuntao, Gao Jian, Li Zhong, Zhang Lei, 2017. Depositional and Provenance Records of Upper Devonian to Lower Carboniferous Sandstones from Bachu Area, Northwestern Tarim Basin: Implications for Tectonic Evolution. Earth Science, 42(3): 421-434. doi: 10.3799/dqkx.2017.032
    Citation: Guo Chuntao, Gao Jian, Li Zhong, Zhang Lei, 2017. Depositional and Provenance Records of Upper Devonian to Lower Carboniferous Sandstones from Bachu Area, Northwestern Tarim Basin: Implications for Tectonic Evolution. Earth Science, 42(3): 421-434. doi: 10.3799/dqkx.2017.032

    塔里木盆地巴楚地区上泥盆统-下石炭统沉积-物源记录及其构造演化

    doi: 10.3799/dqkx.2017.032
    基金项目: 

    国家自然科学基金项目 40972085

    国家重大专项 2011ZX05008-003

    国家自然科学基金项目 41372120

    详细信息
      作者简介:

      郭春涛 (1981-),男,博士,主要从事沉积学研究.ORCID:0000-0001-7861-5062.E-mail:xinylx521@163.com

      通讯作者:

      李忠,ORCID:0000-0001-9155-0742.E-mail:lizhong@mail.iggcas.ac.cn

    • 中图分类号: P542;P597

    Depositional and Provenance Records of Upper Devonian to Lower Carboniferous Sandstones from Bachu Area, Northwestern Tarim Basin: Implications for Tectonic Evolution

    • 摘要: 泥盆纪-石炭纪是南天山洋-塔里木盆地北部陆缘构造演化的关键时期.选取塔里木盆地巴楚地区上泥盆统-下石炭统露头剖面,在沉积体系、碎屑组分、重矿物组合分析基础上,重点通过LA-ICP-MS分析砂岩样品.结果表明,上泥盆统-下石炭统砂岩碎屑颗粒以单晶石英为主,(变质) 结晶岩岩屑极少,物源构造属性主要指示陆块物源区;重矿物组合以锆石、电气石和TiO2矿物等稳定重矿物为主,反映相对远距离的源汇体系和稳定的构造背景;2个年代学样品具有类似的碎屑锆石U-Pb年龄组成和Hf同位素特征,主要反映了383~479 Ma、710~932 Ma、1 752~1 936 Ma、2 419~2 597 Ma共4期构造热事件,并以前两期为主.对比研究显示,上述碎屑物源以塔里木盆地内古隆起为主,同时还可能有来自阿尔金造山带、西昆仑造山带的再旋回沉积.但并没有记录到来自盆地北侧造山带和岛弧的物源信息,说明该时期南天山洋盆并没有闭合,塔里木盆地北缘西部可能不存在洋盆的向南俯冲,晚泥盆世-早石炭世其可能为被动大陆边缘.

       

    • 图  1  巴楚剖面地质简图及碎屑锆石样品点

      改自Yang et al.(2007)

      Fig.  1.  Geological sketch of Bachu area and the position of detrial zircon

      图  2  下石炭统沉积剖面及样品位置

      改自李罗照等 (1996)

      Fig.  2.  The Upper Devonian to Lower Carboniferous depositional column and position of samples of the Bachu outcrop

      图  3  巴楚剖面砂岩正交偏光镜下特征

      BC1-13.上泥盆统东河塘组中细砂岩;BC1-22.上泥盆统甘木里克组中细砂岩;BC3-4.下石炭统巴楚组中细砂岩;BC3-9.下石炭统巴楚组中细砂岩.Qm.单晶石英;Qp.多晶石英;P.斜长石;Ls.(变质) 沉积岩岩屑

      Fig.  3.  Microscopic feature of sandstone of Bachu outcrop

      图  4  巴楚剖面主要岩性、构造

      a.东河塘组冲洗交错层理,东河砂岩沉积构造丰富,发育各种交错层理、水平层理、流水线理、剥离线理等;b.含砾砂岩段滨岸砾岩,砾石以石英质为主,分选磨圆均较好;c.巴楚组下泥岩段土黄色泥岩夹灰绿色粉砂岩,显示低能的潟湖环境;d.巴楚组生屑灰岩段,被压扁的波纹层理,显示台地的波浪作用较强;e.巴楚组中泥岩段小型交错层理;f.巴楚组标准灰岩段,灰岩层中夹河道砂岩,说明有短期的河流注入;g.巴楚组标准灰岩段上部灰岩层,砾屑灰岩极其发育,砾屑分选磨圆均很好,反映高能的沉积环境;h.标准灰岩段上部,灰岩与泥岩薄互层;i.卡拉沙依组,蒸发坪环境,发育厚层的膏岩层,可见粉砂岩夹层

      Fig.  4.  Lithologic and sedimentary structure photographs of the Bachu outcrop

      图  5  巴楚剖面砂岩碎屑组分与物源类型三角图

      Qm.单晶石英;Qp.多晶石英;K.钾长石;P.斜长石;Lv.(变质) 结晶岩岩屑;Ls.(变质) 沉积岩岩屑;Q.总石英颗粒;F.长石;L.不稳定复晶岩屑;Lt.岩屑总含量.改自Dickinson and Suczek (1979)

      Fig.  5.  Triangular plots showing sandstone fragment components and provenance of the Bachu outcrop

      图  6  碎屑锆石样品U-Pb谐和图和年龄频谱

      Fig.  6.  Concordia plots, Histograms and relative probability plots of detrital zircon U-Pb ages

      图  7  碎屑锆石Hf同位素特征

      a.本文碎屑锆石εHf(t) 同位素组成;b.前人报道的εHf(t) 同位素数据汇总 (Long et al., 2010, 2011Ge et al., 2012a, 2012b, 2013Lei et al., 2012)

      Fig.  7.  Hf isotope data of detrital zircons from the two samples

      图  8  碎屑锆石Th/U比值分布

      Fig.  8.  Th/U plots of detrital zircons from the two samples

      图  9  典型碎屑锆石CL照片

      图中圆圈代表原位测试点,直径为32 μm.红色数字为U-Pb年龄,单位为Ma;绿色数字为εHf(t) 值

      Fig.  9.  Typical CL images of detrital zircons

      图  10  样品与潜在物源区构造热事件年龄对比

      a~e引自前人文献 (Dong et al., 2014郭春涛, 2014李忠等, 2015);g和f为本文样品

      Fig.  10.  Comparison of the ages between the samples and possible source areas

      表  1  巴楚剖面砂岩重矿物统计 (%)

      Table  1.   Heavy minerals statistics of sandstone samples in the Bachu outcrop

      样品层位锆石白钛石金红石锐钛矿电气石磷灰石赤褐铁矿镜铁矿
      BC1-13东河塘组50.65.00.826.313.53.7
      BC1-22甘木里克组42.50.91.20.98.845.7
      BC3-9标准灰岩段64.49.90.71.110.913.0
      下载: 导出CSV

      附表 1  巴楚地区碎屑锆石LA-ICP-MS U-Pb测年数据

      附表 1.   Zircon LA-ICP-MS U-Pb dating data from Bachu Area

      样品点232Th/238U同位素比值表面年龄 (Ma)谐和度
      207Pb/206Pb±1σ207Pb/235U±1σ206Pb/238U±1σ207Pb/206Pb±1σ207Pb/235U±1σ206Pb/238U±1σ
      BC1-13-0010.200.055 990.002 710.558 190.025 090.072 300.001 61452614501645010100.0
      BC1-13-0020.560.055 220.007 410.531 460.066 560.069 800.003 82421183433444352399.5
      BC1-13-0030.660.068 670.002 201.312 770.038 500.138 640.002 58889328511783715101.7
      BC1-13-0040.410.163 470.002 1810.631 470.133 990.471 630.006 512 492102 491122 49129100.0
      BC1-13-0050.620.162 090.003 8510.479 180.235 910.468 840.009 892 478172 478212 47843100.0
      BC1-13-0060.970.055 730.002 570.539 210.023 170.070 160.001 4744259438154379100.2
      BC1-13-0070.850.056 210.003 000.551 490.027 340.071 150.001 72461684461844310100.7
      BC1-13-0080.330.066 140.002 981.212 950.050 370.132 990.003 10811498072380518100.2
      BC1-13-0091.180.054 770.011 600.472 170.095 670.062 520.004 244033243936639126100.5
      BC1-13-0100.380.226 880.002 2218.755 420.178 350.599 490.007 333 03093 02993 02830100.1
      BC1-13-0110.170.182 150.003 7612.890 180.254 470.513 180.010 082 673152 672192 67043100.1
      BC1-13-0120.330.064 670.002 671.113 700.042 270.124 890.002 71764457602075916100.1
      BC1-13-0130.420.123 300.002 766.197 620.129 290.364 520.006 542 005172 004182 00431100.0
      BC1-13-0140.770.069 360.003 871.405 870.072 400.147 000.004 18909618913188423100.8
      BC1-13-0150.460.057 360.003 140.606 660.030 610.076 700.001 97505674811947612101.1
      BC1-13-0160.380.056 370.003 210.573 660.030 700.073 800.001 73467774602045910100.2
      BC1-13-0170.930.064 800.004 321.131 050.070 890.126 580.003 67768847683476821100.0
      BC1-13-0180.430.054 810.008 260.492 690.071 400.065 200.002 714043354074940716100.0
      BC1-13-0190.410.071 400.004 871.334 440.083 470.135 540.004 74969728613681927105.1
      BC1-13-0200.690.070 790.002 640.750 980.025 460.076 930.001 5295138569154789119.0
      BC1-13-0210.390.066 980.001 301.283 810.022 900.138 990.001 84837188391083910100.0
      BC1-13-0220.550.067 300.001 421.306 180.025 370.140 760.001 9484720848118491199.9
      BC1-13-0230.160.066 490.002 311.251 220.039 860.136 480.002 6982235824188251599.9
      BC1-13-0240.690.056 330.003 810.576 550.036 780.074 230.002 01465934622446212100.0
      BC1-13-0250.680.111 980.003 735.065 620.155 880.328 060.007 931 832261 830261 82938100.2
      BC1-13-0260.480.064 960.003 351.141 840.054 220.127 480.003 33773577732677319100.0
      BC1-13-0270.360.078 050.003 410.859 580.035 220.079 880.001 211 14889630194957127.3
      BC1-13-0280.680.151 330.006 528.896 900.329 160.426 390.009 442 361752 327342 28943103.1
      BC1-13-0290.290.056 000.004 920.568 340.047 310.073 590.002 40452127457314581499.8
      BC1-13-0301.200.065 890.016 631.178 250.283 640.129 670.011 9780336479013278668100.5
      BC1-13-0310.550.069 190.006 151.392 370.114 730.145 930.006 319041008864987835100.9
      BC1-13-0320.470.153 550.003 159.480 710.183 560.447 770.008 272 386152 386182 38537100.0
      BC1-13-0330.790.057 380.004 370.651 350.046 300.082 320.002 67506100509285101699.8
      BC1-13-0340.670.095 340.006 363.524 300.217 650.268 080.010 831 535601 533491 53155100.3
      BC1-13-0350.620.065 670.002 651.137 020.042 360.125 550.002 66796447712076215101.2
      BC1-13-0360.600.067 410.003 351.310 030.060 200.140 930.003 57850558502685020100.0
      BC1-13-0370.770.066 440.002 871.240 770.049 470.135 420.003 05820478192281917100.0
      BC1-13-0380.880.067 190.006 131.300 260.111 370.140 340.005 68844112846498473299.9
      BC1-13-0390.440.056 250.003 130.572 450.029 790.073 800.001 78462734601945911100.2
      BC1-13-0401.300.055 860.002 750.516 670.023 750.067 080.001 4444764423164199101.0
      BC1-13-0410.570.123 130.005 544.833 850.197 790.284 700.008 972 002341 791341 61545124.0
      BC1-13-0420.520.070 230.003 651.472 000.070 130.152 010.004 24935549192991224100.8
      BC1-13-0430.950.067 830.002 381.339 920.043 580.143 260.002 69863378631986315100.0
      BC1-13-0440.560.065 770.002 241.199 830.037 700.132 300.002 44799368011780114100.0
      BC1-13-0450.630.067 210.003 131.292 050.056 240.139 420.003 16844548422584118100.1
      BC1-13-0460.520.141 960.005 268.168 730.284 260.417 300.012 192 251272 250312 24855100.1
      BC1-13-0470.330.068 200.002 761.317 310.049 000.140 080.003 08875428532184517100.9
      BC1-13-0481.100.066 620.004 101.227 860.071 150.133 650.003 66826768133280921100.5
      BC1-13-0491.100.083 530.008 321.599 180.148 440.138 830.006 361 2821119705883836115.8
      BC1-13-0501.610.174 070.006 2311.872 760.405 520.494 630.015 402 597252 594322 59166100.2
      BC1-13-0510.760.055 260.005 380.517 000.047 530.067 850.002 484231404233242315100.0
      BC1-13-0520.150.057 290.002 280.600 970.022 070.076 070.001 4950347478144739101.1
      BC1-13-0530.450.068 900.001 841.407 020.034 410.148 100.002 41896268921589014100.2
      BC1-13-0540.340.125 910.008 876.321 290.384 490.364 110.012 932 0421282 021532 00261102.0
      BC1-13-0551.430.067 950.003 881.351 390.071 620.144 230.004 0986764868318692399.9
      BC1-13-0561.390.063 400.004 361.043 540.067 170.119 370.003 6272286726337272199.9
      BC1-13-0571.200.087 460.006 481.148 740.077 130.095 240.003 561 371737773658621132.6
      BC1-13-0580.230.145 990.003 468.596 920.191 040.427 040.008 672 299172 296202 29239100.3
      BC1-13-0590.190.070 320.001 831.507 390.035 960.155 460.002 50938259331593114100.2
      BC1-13-0600.620.069 140.001 731.430 800.032 900.150 080.002 35903249021490113100.1
      BC1-13-0610.220.087 350.001 302.843 700.039 060.236 090.002 931 368121 367101 36615100.1
      BC1-13-0620.780.066 870.002 241.273 120.039 210.138 070.002 60834348341883415100.0
      BC1-13-0630.740.065 170.005 521.151 150.090 390.128 090.005 12780997784377729100.1
      BC1-13-0640.420.119 210.003 785.795 420.170 510.352 540.008 371 944241 946251 9474099.8
      BC1-13-0650.750.054 770.005 320.491 620.045 320.065 100.002 30403144406314071499.8
      BC1-13-0660.400.066 480.004 551.264 000.080 070.137 890.004 6082278830368332699.6
      BC1-13-0670.360.116 120.002 505.459 700.108 570.340 970.005 871 897161 894171 89128100.3
      BC1-13-0680.600.065 940.003 291.202 210.055 710.132 220.003 26804578022680119100.1
      BC1-13-0691.000.112 090.010 285.080 210.440 420.328 670.017 541 834841 833741 83285100.1
      BC1-13-0700.260.070 070.003 651.463 340.070 950.151 450.003 93930589152990922100.7
      BC1-13-0710.650.060 190.002 530.790 310.030 540.095 220.002 03610485911758612100.9
      BC1-13-0720.340.129 410.005 736.730 160.277 750.377 140.012 472 090332 077362 06358101.3
      BC1-13-0731.320.065 490.009 191.179 510.158 860.130 610.006 407902037917479136100.0
      BC1-13-0740.250.069 200.002 311.401 530.042 930.146 880.002 82905338901888316100.8
      BC1-13-0750.650.115 500.005 245.408 860.228 190.339 620.010 651 888361 886361 88551100.2
      BC1-13-0760.320.067 010.001 381.284 200.024 400.138 970.001 89838198391183911100.0
      BC1-13-0770.390.189 770.002 9913.863 650.209 620.529 780.008 442 740122 740142 74136100.0
      BC1-13-0780.460.067 630.004 391.309 560.078 070.140 430.004 71857708503484727100.4
      BC1-13-0791.140.120 490.007 375.916 560.339 110.356 100.014 521 963501 964501 9646999.9
      BC1-13-0800.490.056 360.003 820.581 940.036 800.074 880.002 18467894662446513100.2
      BC1-13-0810.210.067 190.002 141.286 600.037 860.138 870.002 46844338401783814100.2
      BC1-13-0820.650.161 120.003 8610.375 770.235 730.467 010.009 942 467172 469212 4704499.9
      BC1-13-0830.770.120 260.005 725.900 210.260 430.355 780.011 791 960371 961381 9625699.9
      BC1-13-0842.000.080 020.002 492.228 800.063 600.202 000.003 911 197281 190201 18621100.9
      BC1-13-0850.390.109 570.004 384.845 460.180 790.320 690.008 521 792331 793311 7934299.9
      BC1-13-0860.390.079 530.007 492.214 160.193 970.201 890.009 791 185991 186611 18553100.0
      BC1-13-0870.220.154 310.002 847.184 300.120 540.337 640.005 492 394132 135151 87526127.7
      BC1-13-0880.830.070 320.004 831.497 090.094 700.154 380.005 43938749293992530100.4
      BC1-13-0890.470.077 010.007 411.368 360.120 090.128 850.006 321 121998755178136112.0
      BC1-13-0900.530.055 750.006 530.546 630.059 800.071 110.003 414421594433944321100.0
      BC1-13-0910.510.119 220.002 705.785 160.121 540.351 900.006 261 945171 944181 94430100.1
      BC1-13-0920.950.065 670.008 921.187 840.152 900.131 160.007 097961817957179440100.1
      BC1-13-0931.120.073 330.003 710.649 500.029 620.064 230.001 651 023525081840110126.7
      BC1-13-0940.370.065 530.002 701.182 830.045 070.130 910.002 81791457932179316100.0
      BC1-13-0951.120.065 810.011 771.201 900.200 290.132 440.010 66800219801928026199.9
      BC1-13-0960.360.055 230.014 160.502 720.123 210.066 010.005 544223644148341234100.5
      BC1-13-0970.590.064 190.004 291.082 010.068 170.122 230.003 48748857453374320100.3
      BC1-13-0980.510.080 090.010 591.816 710.220 930.164 490.011 141 1991371 0518098262107.0
      BC1-13-0990.620.110 330.005 024.917 970.208 310.323 250.009 811 805371 805361 8064899.9
      BC1-13-1000.430.067 570.004 181.315 330.075 000.141 160.004 44855688523385125100.1
      BC1-13-1010.340.069 280.002 491.400 060.046 260.146 550.002 93907378892088216100.8
      BC1-13-1020.460.057 390.002 630.646 880.027 800.081 740.001 63507605071750710100.0
      BC1-13-1030.750.058 980.007 570.512 370.064 030.063 000.001 875662914204339411106.6
      BC1-13-1040.600.068 580.003 601.359 830.065 660.143 790.003 97886568722886622100.7
      BC1-13-1050.520.055 940.002 650.567 460.024 960.073 560.001 6045060456164581099.6
      BC1-13-1060.490.067 040.003 471.282 960.061 330.138 770.003 66839578382783821100.0
      BC1-13-1070.300.066 400.003 041.222 710.051 740.133 550.003 12819508112480818100.4
      BC1-13-1080.530.163 370.005 8610.212 910.299 850.453 400.009 342 491622 454272 41041103.4
      BC1-13-1090.900.064 230.005 260.433 010.034 410.048 890.000 95749179365243086118.5
      BC1-13-1100.650.057 760.004 550.554 350.040 590.069 600.002 335211024482743414103.2
      BC1-13-1110.490.066 900.002 951.250 870.050 620.135 590.003 21835468242382018100.5
      BC1-13-1121.040.083 600.004 132.526 870.115 400.219 190.006 231 283471 280331 27833100.4
      BC1-13-1130.340.100 670.001 954.005 290.071 250.288 530.004 321 636151 635141 63422100.1
      BC1-13-1140.500.054 820.004 360.483 240.036 490.063 930.001 874051174002539911100.3
      BC1-13-1150.410.056 310.002 640.558 000.024 090.071 860.001 60465574501644710100.7
      BC1-13-1160.200.064 960.002 491.141 310.040 520.127 410.002 53773427731977314100.0
      BC1-13-1170.600.056 640.005 470.602 910.054 970.077 190.002 864781374793547917100.0
      BC1-13-1180.750.065 270.007 891.161 400.131 390.129 040.006 877831507836278239100.1
      BC1-13-1190.710.055 130.004 500.498 170.038 590.065 520.001 954171204102640912100.2
      BC1-13-1200.560.064 370.004 401.115 090.070 840.125 630.003 9875481761347632399.7
      BC1-13-1210.470.065 340.007 831.165 960.130 540.129 400.006 817851487856178439100.1
      BC1-13-1220.510.056 130.003 130.565 250.029 300.073 030.001 79458724551945411100.2
      BC1-13-1230.160.075 340.002 401.669 750.046 250.160 750.002 531 078659971896114103.7
      BC1-13-1240.860.066 130.002 601.215 540.043 990.133 300.002 77810428082080716100.1
      BC1-13-1250.410.068 660.003 841.414 220.072 620.149 360.004 3888959895318972599.8
      BC1-13-1260.160.154 390.002 158.490 680.109 390.398 810.005 302 395102 285122 16424110.7
      BC1-13-1270.680.062 990.007 701.011 760.117 290.116 470.005 567081677105971032100.0
      BC1-13-1280.130.071 280.001 841.583 290.037 590.161 080.002 56965249641596314100.1
      BC1-13-1290.500.178 710.002 3812.754 320.161 250.517 550.006 982 641102 662122 6893098.2
      BC1-13-1300.460.072 790.001 741.416 580.030 860.141 140.002 131 008228961385112105.3
      BC1-13-1310.560.161 760.003 1210.442 170.190 290.468 140.008 192 474142 475172 47536100.0
      BC1-13-1320.090.118 520.001 495.644 590.065 590.345 360.004 101 934101 923101 91220101.2
      下载: 导出CSV

      附表 2  巴楚地区碎屑锆石Lu-Hf同位素分析结果

      附表 2.   Zircon Lu-Hf isotope analysis results from Bachu Area

      样品点年龄 (Ma)176Yb/177Hf2σ176Lu/177Hf2σ176Hf/177Hf2σ176Hf/177HfiTDM(Ma)TDMC(Ma)εHf(0)εHf(t)2σfLu/Hf
      BC3-9-0018370.022 2960.001 5400.000 6660.000 0460.281 9140.000 0290.281 9031 8642 509-30.3-12.31.0-0.98
      BC3-9-0028680.020 9430.000 0860.000 6900.000 0040.282 2140.000 0310.282 2031 4521 821-19.7-1.01.1-0.98
      BC3-9-0032 4900.040 6260.000 2650.001 0280.000 0080.281 1870.000 0330.281 1382 8783 138-56.1-1.91.2-0.97
      BC3-9-0041 9360.002 0160.000 0340.000 0420.000 0010.281 4280.000 0210.281 4272 4852 866-47.5-4.40.7-1.00
      BC3-9-0058280.008 3960.000 1150.000 2440.000 0020.282 0180.000 0240.282 0141 7022 268-26.7-8.50.8-0.99
      BC3-9-0074750.020 3300.000 2910.000 6500.000 0080.282 5860.000 0320.282 5809341 220-6.63.71.1-0.98
      BC3-9-0085310.025 9690.000 1360.000 7650.000 0020.282 3480.000 0230.282 3401 2691 725-15.0-3.60.8-0.98
      BC3-9-0091 9120.012 1930.000 0800.000 3540.000 0030.281 2630.000 0270.281 2502 7273 278-53.4-11.21.0-0.99
      BC3-9-0101 9000.002 0130.000 0450.000 0400.000 0010.281 4150.000 0230.281 4142 5032 919-48.0-5.70.8-1.00
      BC3-9-0118530.022 6920.000 0580.000 6760.000 0040.282 2290.000 0240.282 2191 4301 795-19.2-0.70.9-0.98
      BC3-9-0128530.019 1100.000 0300.000 5320.000 0010.281 9540.000 0260.281 9451 8032 406-28.9-10.40.9-0.98
      BC3-9-0135120.019 8280.000 2830.000 5610.000 0110.282 2390.000 0220.282 2341 4121 973-18.8-7.80.8-0.98
      BC3-9-0144330.063 0880.000 6100.001 7750.000 0200.282 5670.000 0290.282 5539891 308-7.21.81.0-0.95
      BC3-9-0152 0900.010 6660.000 2200.000 3170.000 0050.281 5610.000 0220.281 5492 3242 485-42.83.50.8-0.99
      BC3-9-0162 4890.024 1170.000 2490.000 6210.000 0040.281 0390.000 0300.281 0103 0463 428-61.3-6.51.1-0.98
      BC3-9-0177980.023 4880.000 1650.000 6940.000 0050.281 8740.000 0230.281 8641 9192 620-31.7-14.50.8-0.98
      BC3-9-0188790.019 7500.000 0370.000 5890.000 0030.282 2870.000 0260.282 2781 3461 645-17.11.90.9-0.98
      BC3-9-0197310.014 6690.000 3730.000 4170.000 0110.282 3520.000 0250.282 3461 2511 585-14.81.10.9-0.99
      BC3-9-0203370.038 7920.000 3750.000 9790.000 0050.282 7870.000 0310.282 7816588530.57.71.1-0.97
      BC3-9-0212 5210.010 3280.000 1100.000 2880.000 0020.281 0740.000 0270.281 0602 9743 292-60.1-4.01.0-0.99
      BC3-9-0237910.023 4810.000 1300.000 6830.000 0020.282 0260.000 0260.282 0161 7102 287-26.4-9.30.9-0.98
      BC3-9-0248550.070 8490.001 5960.002 1670.000 0480.282 2060.000 0330.282 1711 5221 900-20.0-2.41.2-0.93
      BC3-9-0259230.036 9070.000 0930.000 9860.000 0060.282 1900.000 0250.282 1731 4971 853-20.6-0.80.9-0.97
      BC3-9-0262 5570.024 8450.002 8730.000 6760.000 0750.281 3000.000 0330.281 2672 7002 799-52.14.21.2-0.98
      BC3-9-0274730.026 2960.000 0410.000 7210.000 0010.282 2620.000 0240.282 2561 3861 948-18.0-7.80.9-0.98
      BC3-9-0288910.027 0720.000 2880.000 7430.000 0090.282 1280.000 0280.282 1161 5722 001-22.8-3.51.0-0.98
      BC3-9-0293830.045 3920.000 5180.001 4260.000 0120.282 5720.000 0260.282 5629731 319-7.11.00.9-0.96
      BC3-9-0307140.030 3720.000 6080.000 8080.000 0150.282 0170.000 0270.282 0061 7282 356-26.7-11.30.9-0.98
      BC3-9-0315400.040 3260.000 1880.001 1180.000 0040.282 4740.000 0230.282 4631 1031 443-10.51.00.8-0.97
      BC3-9-0324450.042 2570.000 1570.001 0840.000 0010.282 5190.000 0330.282 5101 0391 398-9.00.51.2-0.97
      BC3-9-0335240.014 8240.000 0900.000 3940.000 0010.282 1930.000 0230.282 1891 4692 065-20.5-9.10.8-0.99
      BC3-9-0344600.013 4810.000 0730.000 3770.000 0010.282 5410.000 0260.282 5379901 326-8.21.80.9-0.99
      BC3-9-0354490.036 2670.000 0720.001 0800.000 0050.282 5330.000 0230.282 5241 0191 363-8.41.10.8-0.97
      BC3-9-0364550.034 8200.000 8810.000 9970.000 0200.282 4230.000 0260.282 4141 1721 606-12.3-2.60.9-0.97
      BC3-9-0372 3460.039 0090.000 1160.001 0220.000 0030.281 4580.000 0290.281 4122 5082 616-46.54.51.0-0.97
      BC3-9-0381 5690.063 1990.000 2970.001 7120.000 0130.281 4960.000 0240.281 4452 5013 066-45.1-12.10.9-0.95
      BC3-9-0394530.055 4790.000 7620.001 4960.000 0150.282 5460.000 0260.282 5331 0121 339-8.01.50.9-0.95
      BC3-9-0408160.023 4600.000 8520.000 6140.000 0140.282 0280.000 0310.282 0181 7052 267-26.3-8.71.1-0.98
      BC3-9-0424670.033 7340.000 9440.001 0470.000 0250.282 5260.000 0230.282 5161 0291 369-8.71.20.8-0.97
      BC3-9-0434930.029 2520.000 1260.000 7590.000 0010.282 0850.000 0260.282 0781 6322 330-24.3-13.70.9-0.98
      BC3-9-0456380.040 3000.000 4230.001 1150.000 0110.282 0680.000 0290.282 0551 6712 294-24.9-11.31.0-0.97
      BC3-9-0464860.034 6970.000 3870.001 1290.000 0140.282 6580.000 0240.282 6488441 060-4.06.30.8-0.97
      BC3-9-0472 5060.015 8720.000 1430.000 4210.000 0030.280 9540.000 0220.280 9343 1443 586-64.3-8.80.8-0.99
      BC3-9-0482 4940.006 1380.000 1080.000 1800.000 0030.280 5600.000 0230.280 5513 6434 445-78.2-22.70.8-0.99
      BC3-9-0494090.028 1330.000 4090.000 8590.000 0110.282 1940.000 0270.282 1881 4862 139-20.4-11.70.9-0.97
      BC3-9-0504630.055 6710.000 3210.001 5600.000 0090.282 5740.000 0270.282 5609741 273-7.02.71.0-0.95
      BC3-9-0517950.012 5290.000 1230.000 3580.000 0030.281 9390.000 0280.281 9341 8152 467-29.5-12.11.0-0.99
      BC3-9-0522 2260.019 7080.000 2010.000 5380.000 0040.281 1860.000 0290.281 1632 8433 262-56.1-7.11.0-0.98
      BC3-9-0535030.061 6960.000 9210.001 6740.000 0230.282 3550.000 0300.282 3391 2901 744-14.8-4.21.0-0.95
      BC3-9-0544630.026 6570.000 5330.000 7000.000 0120.282 1720.000 0260.282 1661 5102 154-21.2-11.20.9-0.98
      BC3-9-0551 8240.029 8250.000 2210.000 9070.000 0040.281 5830.000 0250.281 5522 3302 660-42.0-2.50.9-0.97
      BC3-9-0567460.039 1020.000 5050.001 0700.000 0160.282 0590.000 0250.282 0441 6822 253-25.2-9.30.9-0.97
      BC3-9-0572 4790.001 1000.000 0100.000 0250.000 0000.281 0790.000 0230.281 0782 9483 282-59.9-4.30.8-1.00
      BC3-9-0587900.034 8350.000 5310.000 9050.000 0150.282 0770.000 0250.282 0641 6502 181-24.6-7.60.9-0.97
      BC3-9-0592 4220.029 3720.000 2720.000 7940.000 0080.280 7990.000 0280.280 7623 3824 027-69.8-16.91.0-0.98
      BC3-9-0608290.013 7820.000 3190.000 3830.000 0090.282 0150.000 0270.282 0091 7122 279-26.8-8.71.0-0.99
      BC3-9-0612 1760.028 2890.000 7450.000 9070.000 0270.281 5320.000 0280.281 4952 3992 548-43.83.51.0-0.97
      BC3-9-0627670.011 6980.000 2980.000 3230.000 0080.282 0420.000 0290.282 0371 6732 254-25.8-9.11.0-0.99
      BC3-9-0631 5580.020 7080.000 0710.000 6290.000 0010.281 4440.000 0210.281 4252 5023 117-47.0-13.00.7-0.98
      BC3-9-0644620.013 8970.000 0240.000 3730.000 0010.282 2630.000 0280.282 2601 3721 945-18.0-7.91.0-0.99
      BC3-9-0651 6420.015 5140.000 1660.000 4300.000 0040.281 4790.000 0310.281 4662 4412 972-45.7-9.71.1-0.99
      BC3-9-0677850.031 0180.000 5510.000 9230.000 0150.281 9990.000 0280.281 9851 7592 359-27.3-10.51.0-0.97
      BC3-9-0684490.086 0700.002 8740.002 4240.000 0780.282 4780.000 0310.282 4571 1371 513-10.4-1.21.1-0.93
      BC3-9-0694650.024 2690.000 2510.000 7610.000 0090.282 5120.000 0240.282 5051 0401 396-9.20.80.8-0.98
      BC3-9-0708150.027 2740.000 3050.000 8180.000 0080.282 2850.000 0230.282 2731 3581 697-17.20.30.8-0.98
      BC3-9-0718240.020 8750.000 0190.000 6130.000 0020.282 1370.000 0210.282 1271 5552 018-22.5-4.60.7-0.98
      BC3-9-0724570.018 6920.000 0730.000 5120.000 0010.282 6250.000 0270.282 6208771 141-5.24.71.0-0.98
      BC3-9-0736310.023 5570.000 0260.000 6170.000 0020.281 8680.000 0290.281 8611 9242 728-32.0-18.31.0-0.98
      BC3-9-0747570.022 6910.000 3300.000 6030.000 0080.282 1410.000 0240.282 1321 5492 049-22.3-5.90.9-0.98
      BC3-9-0754590.016 9430.000 2300.000 4600.000 0050.282 5300.000 0270.282 5261 0081 353-8.61.41.0-0.99
      BC3-9-0764690.012 0240.000 1420.000 3330.000 0030.282 4650.000 0300.282 4621 0931 490-10.9-0.61.1-0.99
      BC3-9-0778360.037 6110.000 4440.001 1180.000 0090.282 1410.000 0280.282 1241 5692 018-22.3-4.51.0-0.97
      BC3-9-0781 8110.012 6080.000 0700.000 3500.000 0010.281 3820.000 0200.281 3692 5683 078-49.2-9.30.7-0.99
      BC3-9-0793880.031 0420.000 3020.001 0010.000 0090.282 5200.000 0220.282 5131 0361 427-8.9-0.60.8-0.97
      BC3-9-0817510.048 4900.001 0830.001 4850.000 0220.281 9310.000 0330.281 9101 8812 548-29.8-13.91.2-0.96
      BC3-9-0829320.033 5580.000 2350.000 8820.000 0050.282 0680.000 0230.282 0521 6622 117-24.9-4.90.8-0.97
      BC3-9-0832 4280.027 3190.001 0950.000 7690.000 0310.281 4190.000 0260.281 3832 5452 624-47.85.40.9-0.98
      BC3-9-0848950.004 9630.000 0980.000 1130.000 0030.281 9630.000 0180.281 9611 7712 344-28.6-8.90.6-1.00
      BC3-9-0858390.029 7290.000 0240.000 8590.000 0010.282 3100.000 0210.282 2961 3251 629-16.31.70.8-0.97
      BC3-9-0869750.031 0390.000 1180.000 8020.000 0010.282 0930.000 0220.282 0781 6232 032-24.0-3.00.8-0.98
      BC3-9-0871 5450.049 0140.000 4280.001 4630.000 0170.281 5770.000 0230.281 5352 3722 883-42.2-9.40.8-0.96
      BC3-9-0888270.039 5490.000 8260.001 0300.000 0190.281 9820.000 0240.281 9661 7882 376-27.9-10.30.9-0.97
      BC3-9-0902 3390.012 8240.000 0550.000 3400.000 0010.281 2830.000 0220.281 2682 6992 950-52.7-0.80.8-0.99
      BC3-9-0912 6630.020 5620.000 0380.000 5950.000 0030.281 1330.000 0210.281 1032 9183 095-57.90.80.8-0.98
      BC3-9-0922 5730.027 1230.000 3190.000 7260.000 0060.281 1050.000 0240.281 0692 9663 235-58.9-2.40.9-0.98
      BC3-9-0931 7560.060 3730.000 6020.001 6920.000 0140.281 5850.000 0310.281 5282 3762 758-42.0-4.91.1-0.95
      BC3-9-0942 5140.021 2040.000 2730.000 6640.000 0100.281 1220.000 0270.281 0902 9383 229-58.3-3.10.9-0.98
      BC3-9-0958180.032 6560.000 1250.000 8730.000 0010.282 0810.000 0250.282 0671 6442 156-24.4-6.90.9-0.97
      BC3-9-0964470.042 9780.000 3960.001 1920.000 0110.282 4470.000 0290.282 4371 1441 560-11.5-2.01.0-0.96
      BC3-9-0974720.021 9240.000 0650.000 5820.000 0010.282 5250.000 0260.282 5191 0181 359-8.71.50.9-0.98
      BC3-9-0984750.030 4730.000 1890.000 8390.000 0030.282 2450.000 0290.282 2371 4151 988-18.6-8.51.0-0.97
      BC3-9-0991 8640.109 5160.000 6560.002 8170.000 0060.281 6780.000 0240.281 5782 3152 573-38.7-0.60.9-0.92
      BC3-9-1009250.019 9520.000 4430.000 5220.000 0090.281 7360.000 0230.281 7272 0992 845-36.6-16.50.8-0.98
      BC3-9-1011 0660.028 0960.000 3590.000 7150.000 0080.281 9460.000 0230.281 9311 8232 303-29.2-6.10.8-0.98
      BC3-9-1027770.032 3060.000 3880.000 8660.000 0080.282 1110.000 0250.282 0981 6012 112-23.4-6.70.9-0.97
      BC3-9-1034580.008 7410.000 0730.000 2810.000 0020.281 9240.000 0270.281 9211 8322 697-30.0-20.01.0-0.99
      BC3-9-1044720.080 3600.006 2640.002 1040.000 1560.282 4970.000 0290.282 4781 1001 452-9.70.01.0-0.94
      BC3-9-1058020.008 4300.000 0810.000 2400.000 0030.282 5150.000 0300.282 5111 0221 165-9.18.51.1-0.99
      BC3-9-1061 8120.018 8970.000 4460.000 5150.000 0120.281 3900.000 0250.281 3722 5683 071-48.9-9.10.9-0.98
      BC3-9-1077350.026 0370.000 0420.000 7500.000 0010.282 2160.000 0290.282 2061 4511 898-19.7-3.81.0-0.98
      BC3-9-1082 3510.010 2200.000 1170.000 2570.000 0010.281 0640.000 0250.281 0522 9853 426-60.4-8.20.9-0.99
      BC3-9-1093890.026 8650.000 1210.000 7090.000 0030.282 2790.000 0250.282 2741 3621 958-17.4-9.10.9-0.98
      BC3-9-1101 7520.002 3490.000 0080.000 0510.000 0000.281 4750.000 0240.281 4732 4242 884-45.9-6.90.8-1.00
      BC3-9-1117860.045 1180.001 7380.001 2340.000 0460.282 0540.000 0240.282 0361 6972 246-25.4-8.70.8-0.96
      BC3-9-1124710.040 4860.000 1320.001 0690.000 0020.282 4980.000 0280.282 4881 0681 429-9.70.31.0-0.97
      BC3-9-1136010.025 7890.000 1190.000 6550.000 0040.281 8980.000 0240.281 8901 8852 680-30.9-18.00.9-0.98
      BC3-9-1147990.034 5870.001 3170.000 8830.000 0250.282 2600.000 0240.282 2471 3951 766-18.1-0.90.8-0.97
      BC3-9-1151 3050.025 1650.000 2050.000 6040.000 0030.281 9650.000 0250.281 9511 7902 105-28.5-0.10.9-0.98
      BC3-9-1169180.019 7030.001 8580.000 5160.000 0510.282 1610.000 0260.282 1521 5171 902-21.6-1.60.9-0.98
      BC3-9-1177860.016 6900.000 0490.000 5280.000 0020.282 2460.000 0270.282 2381 4021 794-18.6-1.51.0-0.98
      BC3-9-1188900.028 8480.000 0890.000 8080.000 0010.282 3110.000 0250.282 2981 3211 592-16.32.90.9-0.98
      BC3-9-1191 9030.002 4610.000 0210.000 0670.000 0010.281 4350.000 0260.281 4322 4782 875-47.3-4.90.9-1.00
      BC3-9-1201 9220.009 4630.000 0320.000 2510.000 0000.281 4050.000 0230.281 3962 5302 945-48.3-5.80.8-0.99
      BC3-9-1212 4190.020 5860.000 0350.000 6350.000 0030.281 4520.000 0290.281 4232 4912 540-46.76.61.0-0.98
      BC3-9-1225060.042 1820.000 1210.001 0270.000 0040.282 2440.000 0330.282 2341 4231 977-18.7-7.91.2-0.97
      BC3-9-1232 0240.021 8540.000 2030.000 5290.000 0070.281 2850.000 0290.281 2652 7093 170-52.6-8.11.0-0.98
      BC3-9-1248140.016 4790.000 0530.000 4690.000 0010.282 1800.000 0260.282 1731 4901 923-20.9-3.20.9-0.99
      BC3-9-1257940.023 2610.000 0950.000 6460.000 0010.282 2370.000 0200.282 2271 4181 813-18.9-1.70.7-0.98
      BC3-9-1261 8010.025 8630.000 0470.000 6780.000 0010.281 5020.000 0260.281 4792 4262 838-44.9-5.60.9-0.98
      下载: 导出CSV
    • Carroll, A.R., Graham, S.A., Hendrix, M.S., et al., 1995.Late Paleozoic Tectonic Amalgamation of Northwestern China:Sedimentary Record of the Northern Tarim, Northwestern Turpan, and Southern Junggar Basins.Geological Society of America Bulletin, 107(5):571-594. doi: 10.1130/0016-7606(1995)107<0571:LPTAON>2.3.CO;2
      Carroll, A.R., Graham, S.A., Chang, E.Z., et al., 2001.Sinian through Permian Tectonostratigraphic Evolution of the Northwestern Tarim Basin, China.Geological Society of America Memoir, 194:47-70. http://www.geology.wisc.edu/~carroll/publications/pdf/Carroll%20et%20al.,%202001%20(Kalpin).pdf
      Charvet, J., Shu, L.S., Laurent-Charvet, S., 2007.Paleozoic Structural and Geodynamic Evolution of Eastern Tianshan (NW China):Welding of the Tarim and Junggar Plates.Episodes, 30(3):162-186. https://hal-insu.archives-ouvertes.fr/insu-00179631/file/Junggar_162-172.pdf
      Dickinson, W.R., Suczek, C.A., 1979.Plate Tectonics and Sandstone Compositions.AAPG Bulletin, 63(12):2164-2182.
      Dong, S.L., Li, Z., Xu, J.Q., et al., 2014.Detrital Zircon U-Pb Geochronology and Hf Isotopic Compositions of Middle-Upper Ordovician Sandstones from the Quruqtagh Area, Eastern Tarim Basin:Implications for Sedimentary Provenance and Tectonic Evolution.Chinese Science Bulletin, 59(10):1002-1012.doi: 10.1007/s11434-013-0073-9
      Gao, J., Long, L.L., Qian, Q., et al., 2006.South Tianshan:A late Paleozoic or a Triassic Orogen? Acta Petrologica Sinica, 22(5):1049-1061 (in Chinese with English abstract). https://www.researchgate.net/publication/259241059_South_Tianshan_a_Late_Paleozoic_or_a_Triassic_Orogen
      Gao, J., Long, L.L., Klemd, R., et al., 2009.Tectonic Evolution of the South Tianshan Orogen and Adjacent Regions, NW China:Geochemical and Age Constraints of Granitoid Rocks.International Journal of Earth Sciences, 98(6):1221-1238.doi: 10.1007/s00531-008-0370-8
      Gao, J., Qian, Q., Long, L.L., et al., 2009.Accretionary Orogenic Orocess of Western Tianshan, China.Geological Bulletin of China, 28(12):1804-1816 (in Chinese with English abstract). https://www.researchgate.net/publication/279571465_Accretionary_orogenic_process_of_Western_Tianshan_China
      Ge, R.F., Zhu, W.B., Wu, H.L., et al., 2012a.The Paleozoic Northern Margin of the Tarim Craton:Passive or Active? Lithos, 142-143:1-15.doi: 10.1016/j.lithos.2012.02.010.
      Ge, R.F., Zhu, W.B., Zheng, B.H., et al., 2012b.Early Pan-African Magmatism in the Tarim Craton:Insights from Zircon U-Pb-Lu-Hf Isotope and Geochemistry of Granitoids in the Korla Area, NW China.Precambrian Research, 212-213:117-138.doi: 10.1016/j.precamres.2012.05.001
      Ge, R.F., Zhu, W.B., Wu, H.L., et al., 2013.Timing and Mechanisms of Multiple Episodes of Migmatization in the Korla Complex, Northern Tarim Craton, NW China:Constraints from Zircon U-Pb-Lu-Hf Isotopes and Implications for Crustal Growth.Precambrian Research, 231:136-156.doi: 10.1016/j.precamres.2013.03.005
      Guo, C.T., 2014.Sedimentary Records, Provenance Systems and Paleogeography Reconstruction of Devonian-Carboniferous in Northern Tarim (Dissertation).Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing (in Chinese with English abstract).
      Guo, C.T., Li, Z., Gao, J., et al., 2015.Depositional and Detrital Zircon Geochronological Records of Carboniferous System in Wushi, Northwest Tarim Basin:Implications for Tectonic Evolution.Acta Petrologica Sinica, 31(9):2679-2695 (in Chinese with English abstract). http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20150916
      Guo, Z.F., Liu, X.M., Liu, J., 2004.Sandstone Detrital Composition and Tectonic Setting through Silurian to Devonian in Keping and Bachu Uplift.Henan Petroleum, 18(4):7-10 (in Chinese).
      Han, Y.G., Zhao G.C., Sun, M., et al., 2015.Paleozoic Accretionary Orogenesis in the Paleo-Asian Ocean:Insights from Detrital Zircons from Silurian to Carboniferous Strata at the Northwestern Margin of the Tarim Craton.Tectonics, 34(2):334-351.doi: 10.1002/2014TC003668
      Jia, C.Z., 2004.Stratigraphy of the Tarim Basin and Adjacent Areas:Summary of the Stratigraphy.Science Press, Beijing, 1063 (in Chinese).
      Jiang, C.Y., Mu, Y.M., Zhao, X.N., et al., 2001.Petrology and Geochemistry of an Active Continental-Margin Intrusive Rock Belt on the Northern Margin of the Tarim Plate.Regional Geology of China, 20(2):158-163 (in Chinese).
      Lei, R.X., Wu, C.Z., Chi, G.X., et al., 2012.Petrogenesis of the Palaeoproterozoic Xishankou Pluton, Northern Tarim Block, Northwest China:Implications for Assembly of the Supercontinent Columbia.International Geology Review, 54(15):1829-1842.doi: 10.1080/00206814.2012.678045
      Li, L.Z., Li, Y.B., Xiao, C.T., et al., 1996.The Carboniferous-Permian Stratigraphy of Tarim Basin.Petroleum Industry Press, Beijing, 132 (in Chinese with English abstract).
      Li, Y.J., Mai, G.R., Luo, J.C., et al., 1999.Palaeozoic Tectonic Setting and Provenance Nature Discrimination of Bachu Fault-Uplift, Tarim, Northwest China.Journal of Palaeogeography, 1(4):45-53 (in Chinese with English abstract).
      Li, Y.J., Wang, Z.M., Wu, H.R., et al., 2010.Discovery of Radiolarian Fossils from the Aiketik Group at the Western End of the South Tianshan Mountains of Chinaand Its Implications.Acta Geologica Sinica, 76(2):146-153. doi: 10.1111/acgs.2002.76.issue-2
      Li, Z., Li, R.W., Sun, S., et al., 1999.Detrital Composition and Provenance Tectonic Attributes of Jurassic Sandstones, South Hefei Basin.Acta Petrologica Sinica, 15(3):438-445 (in Chinese with English abstract). https://www.researchgate.net/publication/292220429_Detrital_composition_and_provenance_tectonic_attributes_of_Jurassic_sandstones_south_Hefei_basin
      Li, Z., Peng, S.T., 2010.Detrital Zircon Geochronology and Its Provenance Implications:Responses to Jurassic through Neogene Basin-Range Interactions along Northern Margin of the Tarim Basin, Northwest China.Basin Research, 22(1):126-138.doi: 10.1111/j.1365-2117.2009.00440.x
      Li, Z., Gao, J., Guo, C.T., et al., 2015.Devonian-Carboniferous Tectonic Evolution of Continental Margins in Northern Tarim Block, Northwest China:Constrained by Basin-Fill Sequences and Provenance Systems.Earth Science Frontiers, 22(1):35-52 (in Chinese with English abstract).
      Lin, C.S., Li, S.T., Liu, J.Y., et al., 2011.Tectonic Framework and Paleogeographic Evolution of the Tarim Basin during the Paleozoic Major Evolutionary Stages.Acta Petrologica Sinica, 27(1):210-218 (in Chinese with English abstract). https://www.researchgate.net/publication/285739779_Tectonic_framework_and_paleogeographic_evolution_of_the_Tarim_basin_during_the_Paleozoic_major_evolutionary_stages
      Lin, W., Faure, M., Shi, Y.H., et al., 2008.Palaeozoic Tectonics of the South-Western Chinese Tianshan:New Insights from a Structural Study of the High-Pressure/Low-Temperature Metamorphic Belt.International Journal of Earth Sciences, 98(6):1259-1274.doi: 10.1007/s00531-008-0371-7
      Lin, W., Chu, Y., Ji, W., et al., 2013.Geochronological and Geochemical Constraints for a Middle Paleozoic Continental Arc on the Northern Margin of the Tarim Block:Implications for the Paleozoic Tectonic Evolution of the South Chinese Tianshan.Lithosphere, 5(4):355-381.doi: 10.1130/L231.1
      Liu, J.Y., Lin, C.S., Li, S.T., et al., 2012a.Detrital Zircon U-Pb Geochronology and Its Provenance Implications on Silurian Tarim Basin.Journal of Earth Science, 23(4):455-475.doi: 10.1007/s12583-012-0268-z
      Liu, J.Y., Yang, H.J., Yang, Y.H., et al., 2012b.The U-Pb Chronologic Evidence and Sedimentary Responses of Silurian Tectonic Activities at Northeastern Margin of Tarim Basin.Science China Earth Sciences, 55(9):1445-1460.doi: 10.1007/s11430-012-4466-4
      Long, X.P., Yuan, C., Sun, M., et al., 2010.Archean Crustal Evolution of the Northern Tarim Craton, NW China:Zircon U-Pb and Hf Isotopic Constraints.Precambrian Research, 180(3):272-284.doi: 10.1016/j.precamres.2010.05.001
      Long, X.P., Yuan, C., Sun, M., et al., 2011.The Discovery of the Oldest Rocks in the Kuluketage Area and Its Geological Implications.Science China Earth Sciences, 54(3):342-348.doi: 10.1007/s11430-010-4156-z
      Mattern, F., Schneider, W., 2000.Suturing of the Proto-and Paleo-Tethys Oceans in the Western Kunlun (Xijiang, China):Journal of Asian Earth Sciences, 18, 637-650.doi: 10.1016/S1367-9120(00)00011-0
      Peng, S.T., 2007.Mesozoic-Cenozoic Sedimentary Records of the Piedmont Basins along the Southern and Northern Sides of Tianshan and Its Geodynamic Significance (Dissertation).Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing (in Chinese with English abstract).
      Shu, L.S., Deng, X.L., Zhu, W.B., et al., 2011.Precambrian Tectonic Evolution of the Tarim Block, NW China:New Geochronological Insights from the Quruqtagh Domain.Journal of Asian Earth Sciences, 42(5):774-790.doi: 10.1016/j.jseaes.2010.08.018
      Wang, B., Shu, L.S., Faure, M., et al., 2011.Paleozoic Tectonics of the Southern Chinese Tianshan:Insights from Structural, Chronological and Geochemical Studies of the Heiyingshan Ophiolitic Mélange (NW China).Tectonophysics, 497(1-4):85-104.doi: 10.1016/j.tecto.2010.11.004
      Wu, F.Y., Li, X.H., Zheng, Y.F., et al., 2007.Lu-Hf Isotopic Systematics and Their Applications in Petrology.Acta Petrologica Sinica, 23(2):185-220 (in Chinese with English abstract). http://www.oalib.com/paper/1492671
      Xiao, W.J., Windley, B.F., Liu, D.Y., et al., 2005.Accretionary Tectonics of the Western Kunlun Orogen, China:A Paleozoic-Early Mesozoic, Long-Lived Active Continental Margin with Implications for the Growth of Southern Eurasia.The Journal of Geology, 113(6):687-705.doi: 10.1086/449326
      Xu, J., 2009.Sequence Stratigraphy of Upper Devonian-Carboniferous in Tarim Basin (Dissertation).Central South University, Changsha (in Chinese with English abstract).
      Yang, S.F., Li, Z.L., Chen, H.L., et al., 2007.Permian Bimodal Dyke of Tarim Basin, NW China:Geochemical Characteristics and Tectonic Implications.Gondwana Research, 12(1-2):113-120.doi:: 10.1016/j.gr.2006.10.018
      Yuan, H.L., Gao, S., Liu, X.M., et al., 2004.Accurate U-Pb Age and Trace Element Determinations of Zircon by Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry.Geostandards and Geoanalytical Research, 28(3):353-370.doi: 10.1111/j.1751-908X.2004.tb00755.x
      Zhang, C.L., Zou, H.B., Li, H.K., et al., 2013.Tectonic Framework and Evolution of the Tarim Block in NW China.Gondwana Research, 23(4):1306-1315.doi: 10.1016/j.gr.2012.05.009
      Zhang, L.F., Ai, Y.L., Li, X.P., et al., 2007.Triassic Collision of Western Tianshan Orogenic Belt, China:Evidence from SHRIMP U-Pb Dating of Zircon from HP/UHP Eclogitic Rocks.Lithos, 96(1-2):266-280.doi: 10.1016/j.lithos.2006.09.012
      Zhang, S.B., Gao, Q.Q., 1992.Stratigraphy and Paleontology Through Sinian to Permian in Tarim.Petroleum Industry Press, Beijing, 383 (in Chinese).
      Zhu, Z.X., Li, J.T., Dong, L.H., et al., 2008.Age Determination and Geological Significance of Devonian Granitic Intrusions in Seriyakeyilake Region, Northern Margin of Tarim Basin, Xinjiang.Acta Petrologica Sinica, 24(5):971-976 (in Chinese with English abstract). http://www.oalib.com/paper/1473498
      高俊, 龙灵利, 钱青, 等, 2006.南天山:晚古生代还是三叠纪碰撞造山带?岩石学报, 22(5): 1049-1061. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200605001.htm
      高俊, 钱青, 龙灵利, 等, 2009.西天山的增生造山过程.地质通报, 28(12): 1804-1816. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200912014.htm
      郭春涛, 2014. 塔里木盆地北部泥盆-石炭纪沉积记录与物源演化及构造-古地理重建 (博士学论文). 北京: 中国科学院地质与地球物理研究所, 1-175.
      郭春涛, 李忠, 高剑, 等, 2015.塔里木盆地西北缘乌什地区石炭系沉积与碎屑锆石年代学记录及其反映的构造演化.岩石学报, 31(9): 2679-2695. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201509016.htm
      郭战峰, 刘新民, 刘颉, 2004.塔里木盆地柯坪、巴楚断隆志留-泥盆系砂岩碎屑组分与构造背景关系分析.河南石油, 18(4): 7-10. http://www.cnki.com.cn/Article/CJFDTOTAL-SYHN200404002.htm
      贾承造, 2004.塔里木盆地及周边地层:各纪地层总结各分区地层表.北京:科学出版社, 1063.
      姜常义, 穆艳梅, 赵晓宁, 等, 2001.塔里木板块北缘活动陆缘型侵入岩带的岩石学与地球化学.中国区域地质, 20(2): 158-163. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200102007.htm
      李罗照, 李艺斌, 肖传桃, 等, 1996.塔里木盆地石炭-二叠纪生物地层.北京:石油工业出版社, 132.
      李曰俊, 买光荣, 罗俊成, 等, 1999.塔里木盆地巴楚断隆古生代沉积构造背景和物源区性质的探讨.古地理学报, 1(4): 45-53. http://www.cnki.com.cn/Article/CJFDTOTAL-GDLX199904006.htm
      李曰俊, 孙龙德, 胡世玲, 等, 2003.塔里木盆地塔参1井底部花岗闪长岩的40Ar-39Ar年代学研究.岩石学报, 19(3): 530-536.
      李忠, 李任伟, 孙枢, 等, 1999.合肥盆地南部侏罗系砂岩碎屑组分及其物源构造属性.岩石学报, 15(3): 438-444. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB199903011.htm
      李忠, 彭守涛, 2013.天山南北麓中-新生界碎屑锆石U-Pb年代学记录、物源体系分析与陆内盆山演化.岩石学报, 29(3): 739-755. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201303002.htm
      李忠, 高剑, 郭春涛, 等, 2015.塔里木块体北部泥盆-石炭纪陆缘构造演化:盆地充填序列与物源体系约束.地学前缘, 22(1): 35-52. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201501005.htm
      林畅松, 李思田, 刘景彦, 等, 2011.塔里木盆地古生代重要演化阶段的古构造格局与古地理演化.岩石学报, 27(1): 210-218. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201101014.htm
      彭守涛, 2007. 天山南北山前盆地中-新生代沉积记录及其动力学分析 (博士学位论文). 北京: 中国科学院地质与地球物理研究所.
      许杰, 2009. 塔里木盆地上泥盆统-石炭系层序地层学研究 (博士学位论文). 长沙: 中南大学.
      吴福元, 李献华, 郑永飞, 等, 2007.Lu-Hf同位素体系及其岩石学应用.岩石学报, 23(2): 185-220. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200702002.htm
      张师本, 高琴琴, 1992.塔里木盆地震旦纪至二叠纪地层古生物.北京:石油工业出版社, 383.
      朱志新, 李锦轶, 董连慧, 等, 2008.新疆塔里木北缘色日牙克依拉克一带泥盆纪花岗质侵入体的确定及其地质意义.岩石学报, 24(5): 971-976. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200805005.htm
    • 加载中
    图(10) / 表(3)
    计量
    • 文章访问数:  5913
    • HTML全文浏览量:  2139
    • PDF下载量:  40
    • 被引次数: 0
    出版历程
    • 收稿日期:  2016-09-01
    • 刊出日期:  2017-03-15

    目录

      /

      返回文章
      返回