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Kinematic and tectonic significance of the fold- and fault-related fracture systems in the Zagros Mountains, southern Iran.

机译:伊朗南部扎格罗斯山脉与褶皱和断层有关的断裂系统的运动学和构造意义。

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摘要

Enhancement methods applied on various satellite images (ASTER, ETM and RADAR SAT-1) facilitated the identification and mapping of tectonic fractures in the Zagros fold-and-thrust belt in southwest Iran. The results of the fracture analysis on these enhanced images reveal four principal fracture sets within each fold structure: (i) an axial set defined by normal faults oriented parallel to the fold axial trace, (ii) a cross-axial, extensional fracture set oriented perpendicular to the fold axial trace, (iii) and two sets of intersecting shear fractures, oriented at an acute angle to the cross-axial set. Study of the enhanced images also revealed five fracture sets along the Kazerun fault zone: (i) Riedel R- and R'-shear fracture sets, (ii) extensional T fracture set oriented at a high angle to the trace of the main Kazerun fault, (iii) oblique, synthetic P-shear fracture set, at a low angle to the trace of the main Kazerun fault, and (iv) synthetic Y-shear displacement fracture set, oriented sub-parallel to the main trace of the fault. The estimated mean azimuths of the shortening that developed the fold- and fault-related fracture systems are remarkably close, and are oriented perpendicular to the general NW-SE trend of the Zagros fold-and-thrust belt.; The sampling and analysis of the fold- and fault-related fracture systems were done in a GIS environment. This study shows that an analysis of enhanced satellite images can reveal significant information on the deformation style, timing, and kinematics of the Zagros fold-and-thrust belt. This study suggests that the Zagros orogenic belt, which has mainly been forming since Miocene, due to the convergence of the Iranian and Arabian subplates, has evolved both by thin- and thick-skinned tectonics. Reconfiguration of the Precambrian basement blocks, and the ensuing slip and rotation along the Precambrian faults during the Zagros orogeny, have deformed the folds, and redistributed the fold-related fractures through rigid-body rotation.; Index words. Fracture Analysis, Fold-and Fault-Related Fractures, Kazerun Fault Zone, Lineament Extraction, Image Enhancement Techniques, Fold-and-Thrust Belt, Thin- and Thick-Skinned Tectonics, GIS, Remote Sensing, Zagros, Iran.
机译:应用于各种卫星图像(ASTER,ETM和RADAR SAT-1)的增强方法有助于识别和绘制伊朗西南部Zagros褶皱冲断带的构造裂缝。在这些增强图像上进行的断裂分析结果显示出每个褶皱结构中有四个主要断裂组:(i)由平行于褶皱轴向轨迹定向的正断层定义的轴向组;(ii)取向为横向​​,横向的伸展性断裂组垂直于褶皱轴向痕迹,(iii)和两组相交的剪切裂缝,它们与横向轴线组成锐角。对增强图像的研究还揭示了沿卡泽伦断裂带的五个裂缝集:(i)Riedel R和R'剪切裂缝集,(ii)与主卡泽伦断裂痕迹成高角度的延伸T裂缝集,(iii)与Kazerun主断层迹线成低角度的斜向合成P型剪切裂缝组,以及(iv)与断层主迹平行的取向的Y型剪切位移综合裂缝组。形成褶皱和断层相关断裂系统的缩短期的估计平均方位角非常接近,并且垂直于Zagros褶皱冲断带的总体NW-SE趋势。褶皱和断层相关断裂系统的采样和分析是在GIS环境中完成的。这项研究表明,对增强型卫星图像的分析可以揭示有关Zagros褶皱冲断带变形形式,时间和运动学的重要信息。这项研究表明,由于伊朗和阿拉伯亚板块的汇聚,自中新世以来主要形成的扎格罗斯造山带已由薄皮构造和厚皮构造演化。前寒武纪基底块的重新构造,以及随后在Zagros造山运动中沿前寒武纪断层滑动和旋转,使褶皱变形,并通过刚体旋转重新分布了与褶皱有关的裂缝。索引词。断裂分析,与褶皱和断裂有关的断裂,Kazerun断裂带,线质提取,图像增强技术,褶皱和冲断带,薄皮和厚皮构造,GIS,遥感,伊朗扎格罗斯。

著录项

  • 作者

    Mobasher, Katayoun.;

  • 作者单位

    Georgia State University.;

  • 授予单位 Georgia State University.;
  • 学科 Geology.
  • 学位 Ph.D.
  • 年度 2007
  • 页码 143 p.
  • 总页数 143
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地质学;
  • 关键词

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