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    准东构造隆升对砂岩型铀成矿作用的制约:磷灰石裂变径迹证据

    宋继叶 秦明宽 蔡煜琦 郭强 何中波 刘章月 曹煦 陈志国

    宋继叶, 秦明宽, 蔡煜琦, 郭强, 何中波, 刘章月, 曹煦, 陈志国, 2019. 准东构造隆升对砂岩型铀成矿作用的制约:磷灰石裂变径迹证据. 地球科学, 44(11): 3910-3925. doi: 10.3799/dqkx.2018.331
    引用本文: 宋继叶, 秦明宽, 蔡煜琦, 郭强, 何中波, 刘章月, 曹煦, 陈志国, 2019. 准东构造隆升对砂岩型铀成矿作用的制约:磷灰石裂变径迹证据. 地球科学, 44(11): 3910-3925. doi: 10.3799/dqkx.2018.331
    Song Jiye, Qin Mingkuan, Cai Yuqi, Guo Qiang, He Zhongbo, Liu Zhangyue, Cao Xu, Chen Zhiguo, 2019. Uplift-Denudation of Orogenic Belts Control on the Formation of Sandstone Type Uranium (U) Deposits in Eastern Junggar, Northwest China: Implications from Apatite Fission Track (AFT). Earth Science, 44(11): 3910-3925. doi: 10.3799/dqkx.2018.331
    Citation: Song Jiye, Qin Mingkuan, Cai Yuqi, Guo Qiang, He Zhongbo, Liu Zhangyue, Cao Xu, Chen Zhiguo, 2019. Uplift-Denudation of Orogenic Belts Control on the Formation of Sandstone Type Uranium (U) Deposits in Eastern Junggar, Northwest China: Implications from Apatite Fission Track (AFT). Earth Science, 44(11): 3910-3925. doi: 10.3799/dqkx.2018.331

    准东构造隆升对砂岩型铀成矿作用的制约:磷灰石裂变径迹证据

    doi: 10.3799/dqkx.2018.331
    基金项目: 

    国防预研项目 3210402

    国防科工局核能开发科研项目 D1302

    详细信息
      作者简介:

      宋继叶(1982—), 女, 高级工程师, 博士, 现主要从事砂岩型铀成矿规律和成矿预测方面的工作

    • 中图分类号: P612

    Uplift-Denudation of Orogenic Belts Control on the Formation of Sandstone Type Uranium (U) Deposits in Eastern Junggar, Northwest China: Implications from Apatite Fission Track (AFT)

    • 摘要: 通过实测磷灰石裂变径迹方法,并结合前人研究结果,分析了准东构造隆升特征,探讨了其与地层沉积、构造响应及对砂岩型铀成矿的制约.研究表明,210~180 Ma,准东缘卡拉麦里地区持续隆升遭受剥蚀,而卡拉麦里山北部奥克什山地区隆升-剥蚀时间相对较晚,于160~80 Ma快速隆升,该期快速隆升控制了五彩湾-老君庙-将军庙与卡姆斯特地区沉积地层发育、古水流方向、区域不整合与构造掀斜等,从而控制着2个地区的砂岩型铀矿成矿条件.五彩湾-老君庙-将军庙地区下侏罗统物源充足、砂体与氧化发育,是该地区主要找矿目的层,而卡姆斯特地区随着晚侏罗世-晚白垩世,盆地东北部奥克什山乃至青格里底山的隆升,增加了物源供给,下侏罗统沉积地层在该地区表现出了更好的成矿潜力.

       

    • 图  1  准噶尔盆地及邻区构造地质单元与构造格架划分

      何登发等(2012)修改.1.中-新生代覆盖区;2.蛇绿岩或超基性岩带;3.板块碰撞带;4.地壳俯冲带;5.国界线;6.主要断裂编号:①额尔齐斯断裂;②中天山北缘断裂;③中天山南缘断裂;④南天山山脉断裂

      Fig.  1.  Geotectonic map showing the tectonic geological unit and structural framework of Junngar basin and its adjacent areas

      图  2  准噶尔盆地东缘地质构造略图与地质剖面及采样位置

      何登发等(2012)修改.1.新生界;2.白垩系;3.侏罗系;4.三叠系;5.前古生界基底;6.花岗岩;7.逆冲推覆断层;8.断层;9.断裂编号;10.泉水;11.国界;12.采样位置; 其中,D402/1-5为李玮(2007)分析样品

      Fig.  2.  Sketch geological map and sample locations of Eastern Junggar basin

      图  3  准噶尔西北缘、东北缘奥克什山锆石裂变径迹分析数据

      李玮(2007)

      Fig.  3.  Zircon fission track data of samples from northwestern and northeastern margins of Junggar basin

      图  4  准噶尔盆地东缘卡拉麦里地区样品磷灰石裂变径迹单颗粒年龄分布

      Fig.  4.  Single grain age distributions of apatite fission track of samples from Kalamaili area, Eastern Junngar

      图  5  准噶尔东缘奥克什山磷灰石裂变径迹单颗粒年龄分布

      李玮(2007)

      Fig.  5.  Single grain age distribution of apatite fission track of samples from Aokeshi area, Eastern Junngar

      图  6  准噶尔东缘卡拉麦里地区磷灰石裂变径迹长度分布和单颗粒年龄放射图

      Fig.  6.  Apatite fission-track length feature and single grain age curiegrams of samples from Kalamaili area, Eastern Junngar

      图  7  准噶尔东缘奥克什山典型样品磷灰石裂变径迹反演模拟的时间温度曲线

      李玮(2007)

      Fig.  7.  Temperature-time modeling results of typical samples based on the apatite fission track dating PAZ-partial annealing zone from Aokeshi area, Eastern Junngar

      图  8  准噶尔东缘帐篷沟地区J1b/T1+2c以及K/J3sh之间的不整合接触关系

      Fig.  8.  Photos of unconformity contact relationship between J1b and T1+2c and K and J3sh of Zhangpenggou area, Eastern Junngar

      图  9  准噶尔东缘卡拉麦里山南侧至博格达山构造地质剖面

      何登发等(2012)修改;剖面位置见图 2B-B’所示

      Fig.  9.  Structural geological section from the south side of Kalamaili mountain to the north side of Bogeda mountain, Eastern Junngar

      图  10  准噶尔东缘卡拉麦里山北侧卡姆斯特地区构造地质剖面

      赵淑娟等(2014)修改;剖面位置如图 2A-A’所示

      Fig.  10.  Structural geological section of Kamusite area on the north side of Kalamaili mountain, Eastern Junngar

      图  11  准噶尔盆地下侏罗统八道湾组沉积体系

      Fig.  11.  Diagram showing Badaowan Formation sedimentary system of Lower Jurassic in Junngar basin

      图  12  准噶尔盆地下侏罗统三工河组沉积体系

      Fig.  12.  Diagram showing Sangonghe Formation sedimentary system of Lower Jurassic in Junngar basin

      图  13  准噶尔盆地中侏罗世西山窑组沉积体系

      Fig.  13.  Diagram showing Xishanyao Formation sedimentary system of Middle Jurassic in Junngar basin

      图  14  准噶尔盆地中侏罗世头屯河组沉积体系

      Fig.  14.  Diagram showing Toutunhe Formation sedimentary system of Middle Jurassic in Junngar basin

      表  1  准噶尔盆地东缘样品裂变径迹数据

      Table  1.   Fission track data of the sample from the eastern margin of Junggar basin

      实验编号 原始编号 海拔(m) 样品位置 岩性 颗粒数(个) ρs(105/cm2Ns ρi(105/cm2Ni ρd(105/cm2Nd P2) (%) 中值年龄±1σ (Ma) 池年龄±1σ (Ma) L(μm) N
      186 JE14-35 1 205 卡拉麦里山 花岗闪长岩 32 19.049 (4 715) 26.216 (6 489) 10.766 (5 864) 0 158±10 158±8 13.5±2.4 (135)
      187 JE14-59 874 凝灰质细砂岩 35 3.184 (776) 3.784 (922) 11.615 (5 864) 99.7 197±13 197±13 13.9±2.1 (100)
      188 JE14-60 874 闪长岩 20 3.666 (284) 5.745 (445) 9.487 (5 864) 35.7 123±12 123±11 14.6±1.8 (56)
      189 JE14-62 975 闪长玢岩 35 1.62 (491) 2.316 (702) 11.463 (5 864) 85 162±12 162±12 13.4±2.1 (69)
      李丽等(2008) 03-45 1 224 花岗岩 24 1.987 (316) 9.98 (1 586) 13.54 (3 372) 0 43.2±4.7 \ 12.37±0.22 (61)
      03-46 1 189 24 1.483 (201) 7.71 (1 045) 13.53 (3 369) 0.9 41.6±4.7 \ 12.82±0.26 (60)
      03-47-2 1 475 24 16.010 (1 497) 22.01 (2 058) 13.52 (3 366) 8.5 \ 171.0±15.5 12.99±0.23 (62)
      李玮(2007) D407-1 1 580 奥克什山 花岗岩 25 1.731 (297) 4.720 (810) 9.340 (10 438) 99.8 66±5 66±5 12.6±2.2 (102)
      D407-2 1 538 22 2.457 (293) 8.586 (1 024) 9.442 (10 438) 14.1 52±4 52±4 12.8±2.7 (123)
      D407-3 1 470 24 1.419 (288) 4.257 (864) 9.545 (10 438) 46.8 61±5 61±5 11.7±2.4 (117)
      D407-4 1 408 25 3.215 (351) 9.984 (1 090) 9.648 (10 438) 99.1 60±4 60±4 11.9±2.6 (77)
      D407-5 1 328 24 1.998 (321) 6.025 (973) 9.751 (10 438) 72.1 62±4 62±4 11.2±2.6 (104)
      注:P2)为自由度(n-1)χ2值的几率,ρs、ρi和ρd分别为自发径迹密度、诱发径迹密度和标准径迹密度;NsNiNd分别为自发径迹数、诱发径迹数和标准径迹数;L为径迹长度.样品测试由北京市泽康恩科技有限公司完成,实验条件为:在25 ℃下用7%HNO3蚀刻30 s揭示自发径迹,将低铀白云母外探测器与矿物一并入反应堆辐照,之后再在25 ℃下用40%HF蚀刻20 s揭示诱发径迹,中子注量利用CN5铀玻璃标定.
      下载: 导出CSV
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