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    长春东南劝农山地区早二叠世范家屯组岩石变形组构及流变学特征

    梁琛岳 刘永江 朱建江 李伟民 常瑞虹 张丽

    梁琛岳, 刘永江, 朱建江, 李伟民, 常瑞虹, 张丽, 2017. 长春东南劝农山地区早二叠世范家屯组岩石变形组构及流变学特征. 地球科学, 42(12): 2174-2192. doi: 10.3799/dqkx.2017.139
    引用本文: 梁琛岳, 刘永江, 朱建江, 李伟民, 常瑞虹, 张丽, 2017. 长春东南劝农山地区早二叠世范家屯组岩石变形组构及流变学特征. 地球科学, 42(12): 2174-2192. doi: 10.3799/dqkx.2017.139
    Liang Chenyue, Liu Yongjiang, Zhu Jianjiang, Li Weimin, Chang Ruihong, Zhang Li, 2017. Deformation Fabrics and Rheological Features of Early Permian Fanjiatun Formation from Quannongshan Area, Southeastern Changchun. Earth Science, 42(12): 2174-2192. doi: 10.3799/dqkx.2017.139
    Citation: Liang Chenyue, Liu Yongjiang, Zhu Jianjiang, Li Weimin, Chang Ruihong, Zhang Li, 2017. Deformation Fabrics and Rheological Features of Early Permian Fanjiatun Formation from Quannongshan Area, Southeastern Changchun. Earth Science, 42(12): 2174-2192. doi: 10.3799/dqkx.2017.139

    长春东南劝农山地区早二叠世范家屯组岩石变形组构及流变学特征

    doi: 10.3799/dqkx.2017.139
    基金项目: 

    国家自然科学基金项目 41230206

    国家自然科学基金项目 41602211

    详细信息
      作者简介:

      梁琛岳(1986-), 男, 讲师, 主要从事构造地质学与岩石流变学研究

      通讯作者:

      刘永江

    • 中图分类号: P542

    Deformation Fabrics and Rheological Features of Early Permian Fanjiatun Formation from Quannongshan Area, Southeastern Changchun

    • 摘要: 劝农山地区位于长春市东南部,处于佳-伊断裂和西拉木伦河缝合带交汇处.详细野外调查发现,该区曾遭受强烈韧性剪切变形,剪切带内岩石普遍糜棱岩化,主要由下二叠统范家屯组(P1f)钙质糜棱岩与侵入其中的燕山期花岗质糜棱岩组成,变形程度处于初糜棱岩至糜棱岩之间,多具有糜棱结构.岩石应变类型主要为压扁型应变,偏一般压缩,为L=S型构造岩,指示其形成于挤压型剪切带的构造环境.多种宏微观韧性剪切变形标志,指示明显的左行剪切运动.电子探针方解石-白云石地质温度计、方解石和石英EBSD组构特征、方解石e双晶形态以及石英长石变形行为等均显示岩石具有低温塑性流变特点,变形环境不超过绿片岩相.剪切带内应变速率偏高,应变集中带应变速率最大,在10-6.95~10-8.89之间,远离强变形带应变速率在10-9.25~10-12.17之间,糜棱岩化作用过程中差异应力下限应大致为51.27~65.46 MPa,代表剪切带糜棱岩化作用为低温中等强度应变,在稍快的应变速率条件下形成.压溶扩散和双晶滑移为劝农山韧性剪切带变形初期的主要变形机制,随着递进变形,逐渐以双晶滑移和晶内滑移为主,递进变形晚期,局部强变形域内发生了粒间滑移.劝农山韧性剪切带形成与早白垩世中晚期伊泽纳崎板块NNW向高斜度斜向俯冲于欧亚大陆之下有关,是佳-伊断裂带左旋走滑事件的局部表现.

       

    • 图  1  长春市劝农山地区地质简图(据1:20万长春幅地质图修改)与采样位置

      a.研究区大地位置简图;b.研究区及周边地质简图;a.西拉木伦河断裂带;b.佳-伊断裂带;c.敦-密断裂带

      Fig.  1.  Geological map of Quannongshan areawith sample locations

      图  2  劝农山韧性剪切带构造剖面图

      Fig.  2.  The structural cross-section of the Quannongshan ductile shear zone in southeastern Changchun

      图  3  宏观构造变形特征

      a.钙质糜棱岩中片麻理发育(795QN-1);b.生物碎屑灰岩(弱变形;855QN-1);c.碎屑灰岩中发育的书斜式构造和眼球状构造,指示NE向左旋剪切运动;d.花岗质糜棱岩中的石英拉长条带(852SJ-1);e.钙质糜棱岩中的不对称褶皱,指示左旋剪切;f.钙质糜棱岩(灰岩)中的膝折

      Fig.  3.  The representative meso-fabrics

      图  4  韧性剪切带典型显微构造变形特征

      a.长眼球状方解石扭折变形,指示左行剪切变形(795QN-1);b.钾长石旋转残斑,边部细粒化,形成核幔结构,具有左行剪切特征(852SJ-1);c.钾长石旋转残斑指示左行剪切,石英波状消光,可见膨凸式动态重结晶(852SJ-1);d.石英颗粒发生膨凸式动态重结晶(852SJ-1);e.残斑方解石机械双晶发育,解理弯曲现象明显(855QN-1);f.方解石残斑书斜式构造具有左行剪切特征(855QN-1);g.方解石旋转残斑指示左行剪切(857QN-1);h.缝合线(压溶面)构造,指示应力方向,SE-NW向挤压(857QN-1);Qtz.石英;Kf.钾长石;Cal.方解石

      Fig.  4.  Typical microscopic deformation characteristics

      图  6  韧性剪切带矿物晶格优选定向

      为下半球等面积投影;X0.拉伸线理方向;Z0.面理法线;N.测量点数;石英C轴组构指示左旋剪切运动类型

      Fig.  6.  LPOs of minerals from the typical mylonites

      图  5  韧性剪切带内典型样品石英和方解石的有限应变Flinn参数图解

      a.岩石有限应变Flinn判别图解;b.岩石变形强度Flinn图解;据郑亚东和常志忠(1985)

      Fig.  5.  Flinn parameters diagram of finite strain of quartz and calcite in the typical mylonites

      图  7  韧性剪切带内钙质糜棱岩方解石电子探针分析位置

      图b中1~7点号是图a方解石颗粒

      Fig.  7.  The positions of electron probe analysis of calcite in calc-mylonites

      图  8  方解石双晶纹密度、宽度与温度关系

      Ferrill et al.(2004)

      Fig.  8.  Relationship between density, width of calcite twin lamellae and temperature

      表  1  韧性剪切带内典型样品显微构造特征

      Table  1.   Microtectonic features of oriented thin sections from Quannongshan ductile shear zone

      样品号岩性采样位置结构构造微观变形特征
      795QN-1钙质糜棱岩N:43°47′17.6″
      E:125°41′37.0″
      鳞片变晶结构
      片状构造
      糜棱岩化,方解石解理塑性弯曲变形,机械双晶与旋转残斑发育,多呈长眼球状,显示左旋特征.基质为细粒新晶方解石.
      852SJ-1花岗质糜棱岩N:43°50′21.2″
      E:125°43′37.5″
      糜棱结构
      片状构造
      长石残斑环状消光,部分绢云母化,长石旋转残斑显示左旋剪切特征;细粒石英拉长成条带,部分石英残斑拉长呈眼球状且细粒化,发育膨凸式动态重结晶.云母片状定向排列.
      855QN-1钙质糜棱岩N:43°47′30.7″
      E:125°41′04.5″
      鳞片变晶结构
      片状构造
      残斑方解石呈长眼球状,机械双晶发育,解理有扭折和弯曲现象,部分边部产生亚颗粒式重结晶.新晶多呈小椭球状,无解理,构成核幔结构.部分方解石颗粒受剪切应力形成书斜式构造,与旋转残斑一致,都显示左旋剪切的特征.
      857QN-1钙质糜棱岩鳞片变晶结构
      片状构造
      方解石残斑长眼球状,旋转变形,指示左旋变形.残斑周边新晶方解石呈长条状或粒状,多呈定向排列.
      下载: 导出CSV

      表  2  韧性剪切带内典型样品石英和方解石的有限应变测量分析数据

      Table  2.   Finite strain measurement analysis data of quartz and calcite in the typical mylonites

      样品号测试颗粒颗粒长短轴法
      X/ZY/ZX/Y菲林指数(k)应变强度(γ)
      852SJ-1石英石英691.351.181.140.811.32
      795QN-1方解石方解石残斑751.791.441.240.601.68
      855QN-1方解石变形鲕粒351.771.391.270.731.66
      855QN-1方解石方解石残斑452.111.631.290.531.92
      857QN-1方解石方解石残斑391.981.561.270.541.83
      下载: 导出CSV

      表  3  韧性剪切带内矿物晶格优选方位EBSD测试结果

      Table  3.   EBSD-measured results of the typical mylonites

      样品号岩性测试矿物EBSD测点数量组构类型剪切指向温度估算(℃)
      795QN-1钙质糜棱岩方解石961e1双晶滑动(80~800 ℃),与r1平移滑动(300~400 ℃)左旋剪切80~400
      855QN-1钙质糜棱岩方解石409e1双晶滑动(80~800 ℃),与r1平移滑动(300~400 ℃)左旋剪切80~400
      852SJ-1花岗质糜棱岩石英213底面<a>滑移为主,局部表现菱面<a>组构主体<400,局部400~550
      下载: 导出CSV

      表  4  韧性剪切带内钙质糜棱岩中方解石电子探针成分数据(%)及温度计算

      Table  4.   Electron probe composition (%) data and calculated temperature of calcite in calc-mylonites

      样品号测点TiO2CaOK2ONa2OMgOAl2O3SiO2FeOMnOCr2O3TotalT(℃)
      1052.76000.040.8300.02000.1100.0800.03053.870366
      2057.05000.030.6600.1100.2900.4000.2600.01058.810312
      3054.3000.0300.100.4200.0100.0300.0500.1300.02055.090186
      4057.2500.0300.030.360000.1900.0700.02057.950118
      50.0653.3800.2800.030.530000.0800.120054.470262
      855QN-16053.45000.010.4600.03000.2600.210054.420235
      7054.9000.0300.010.850000.4700.090056.340373
      80.03255.8440.0080.0160.56700.0130.2060.2490.00656.941275
      9052.5520.00600.7410.00100.1300.0060.02853.464346
      100.01456.9510.0230.0490.465000.1090.0580.03857.707209
      11055.3980.0440.0040.6060.04100.0990.086056.278289
      平均温度(℃)270
      12056.0250.0200.0470.3800.0310.0240.2060.201056.934147
      857QN-1130.00555.4530.02000.308000.0310.018055.83544
      14055.4680.0310.0340.3270.01300.1270.0140.03856.05281
      平均温度(℃)91
        注:电子探针实验是在吉林大学东北亚矿产资源评价国土资源部重点实验室电子探针实验室完成,实验仪器为日本电子公司JXA 8230型电子探针仪,电子束流为1×10-8 A,加速电压15 kV,电子束斑为2 μm,修正方法为ZAF法.
      下载: 导出CSV

      表  5  韧性剪切带内钙质糜棱岩中方解石双晶统计

      Table  5.   Electron probe composition (%) data and calculated temperature of calcite in calc-mylonites

      样品号颗粒数平均双晶宽度(μm)平均双晶密度(条/mm)Ⅰ型Ⅱ型Ⅲ型Ⅳ型估算Tmax(℃)
      795QN-1371.4351.6162100170~200
      855QN-1572.5732.91823151>250
      857QN-1221.1154.516600170~200
      下载: 导出CSV

      表  6  韧性剪切带内糜棱岩方解石古差应力及应变速率估算

      Table  6.   Estimation of Paleo-stress and strain rates

      样品号变形温度(℃)统计颗粒数动态重结晶颗粒平均粒度
      粒径D(μm)
      应力计(MPa)
      Twiss(1977)
      σ=750D-0.68
      应变速率(s-1)
      Heard and Raleich(1972)
      795QN-1804040.360.7410-11.56
      2004040.360.7410-9.25
      855QN-12004536.165.4610-8.98
      4004536.165.4610-6.95
      857QN-1804051.751.2710-12.17
      2004051.751.2710-9.86
      下载: 导出CSV

      表  7  利用方解石e双晶发育程度估算古差异应力值

      Table  7.   Differential stress inferred by use of calcite e-twin lamellaes

      样品号具有双晶颗粒的数目双晶化颗粒百分数(%)分解剪切应力系数S1古差异应力值σ(MPa)
      一组双晶两组双晶不具双晶颗粒总数一组双晶两组双晶一组双晶两组双晶一组双晶两组双晶
      795QN-128643873.6815.790.130.1676.9262.50
      855QN-133895066.0016.000.190.1652.6362.50
      857QN-115352365.2213.040.200.1850.0055.56
      下载: 导出CSV
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