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吉林中部断裂构造带的基本特征及其形成演化的研究
引用本文:张寿德,邵学君.吉林中部断裂构造带的基本特征及其形成演化的研究[J].吉林地质,2013(4):31-34.
作者姓名:张寿德  邵学君
作者单位:[1]吉林省第二地质调查所,吉林吉林市132013 [2]吉林省地质调查院,吉林长春130061
摘    要:吉林中部断裂构造带位于梨树断陷东侧,断裂构造带包括南金山断裂、北金山断裂、吉林中部断裂、苏家屯断裂。本文介绍了火石岭期、沙河子期、营城期、登娄库期—泉头早期、嫩江期末期—明水期和喜马拉雅期,南金山断裂、北金山断裂、吉林中部断裂、苏家屯断裂构造形、成演化史。

关 键 词:吉林中部断裂带  梨树断陷  结构构造  形成演化

Basic features and its formation and evolution of middle part of Jilin fault zone
ZHANG Shou-de;SHAO Xue-jun.Basic features and its formation and evolution of middle part of Jilin fault zone[J].Jilin Geology,2013(4):31-34.
Authors:ZHANG Shou-de;SHAO Xue-jun
Institution:ZHANG Shou-de;SHAO Xue-jun;The Second Geological Survey of Jilin Province;Institute of Geological Survey of Jilin Province;
Abstract:Jilin central fault zone is located in the east of Lishu fault depression,including the South Jinshan fault,North Jinshan fault,middle part of Jilin fault,Sujiatun fault.In this paper,introduces tectonic formation and evolution of Huoshiling stage,Shahezi stage,Yingcheng stage,Denglouku stage- early phase of Quantou,last phase of Nenjiang- Mingshui stage and Himalayan,South Jinshan fault,North Jinshan fault,middle part of Jilin fault,Sujiatun fault.
Keywords:Middle part of Jilin fault zone  Lishu fault depression  structure  formation and evolution
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