ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
鲁西青邑韧性剪切带运动学涡度及剪切作用类型
  
关键词:kinematic vorticity  type of shear  three-dimensional deformation  Qingyi ductile shear zone
基金项目:国家自然科学基金项目(编号:40102017)和原地质矿产部“1:5万田黄、土旺幅区域地质调查”项目
作者单位E-mail
王新社 中国地质科学院地质研究所,北京100037 xinshewang@cags.net.cn 
张尚坤 中国地质大学地球科学与资源学院,北京100083  
张富中 山东省地质调查院,山东济南250013  
杨崇辉 中国地质科学院地质研究所,北京100037  
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摘要:
Kinematic Vorticities and Shear Types of the Qingyi Ductile Shear Zone in Western Shandong
      The Qingyi ductile shear zone (QDSZ) developed in Late Archean is a large-size ductile shear zone in granite of the western Shandong Precambrian basement. The QDSZ trends NW-SE with nearly vertical foliation and subhorizontal lineation. The shear indicators and quartz c-axial fabrics in the zone imply dextral strike-shearing. Kinematic vorticity numbers in the QDSZ obtained through quartz C-axial fabrics analysis range from 0.96 to 0.99. Kinematic vorticity numbers given by polar Mohr constructions of mylonitic rocks, protomylonite, mylonite and ultramylonite are 0.91,0.87,0.81 and 0.60, respectively. Kinematic vorticity numbers show that the shear type of the QDSZ was at first a general shear, and the pure shear component gradually increased with deformation. Analyses of the shear type and the three-dimensional deformation demonstrate that the QDSZ belongs to a lengthening-broadening shear zone with the lengthening quite obvious along the Y-axis. This means that ductile shearing played a role of crust-thickening du-(ring) the cratonization at the end of Archean.
WANG Xin-she,ZHANG Shang-kun,ZHANG Fu-zhong,YANG Chong-hui.2005.Kinematic Vorticities and Shear Types of the Qingyi Ductile Shear Zone in Western Shandong[J].Acta Geoscientica Sinica,26(5):423-428.
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