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贵州镇宁沙子沟地区北西向构造形迹及特征
引用本文:王筑生.贵州镇宁沙子沟地区北西向构造形迹及特征[J].贵州地质,2000,17(1):30-33,39.
作者姓名:王筑生
作者单位:贵州地勘局贵阳 550004
摘    要:沙子沟地区北西向构造是省内闻名的水城-紫云变形带向南东方向的延伸段,该北西向构造带除褶皱外,尚发育有一毓的逆冲断层构造,为一个大型的褶皱断裂构造带。它由两个褶皱带和个部断层带组成,即:打邦-六马-打万挤压褶皱带、阐益-乐纪-岜解逆冲断层带、店子上-岜闹褶皱带、白石岩-板逆冲断层带。

关 键 词:贵州  沙子沟地区  北西向  构造形迹  构造特征
文章编号:1000-5943(2000)01-0030-05

Characteristics of the North - Westward Structure of Shazigou District in Zhenling, Guizhou
WANG Zhu_shen.Characteristics of the North - Westward Structure of Shazigou District in Zhenling, Guizhou[J].Guizhou Geology,2000,17(1):30-33,39.
Authors:WANG Zhu_shen
Abstract:North-westward structure of Shazigou area is located in the south-east extended member of the well-known Shuicheng-Ziyun deformation zone of Guizhou. Except for the fold in the north-westward structural zone, still series of overthrust structure have developed as a folded-faulted macrostructral belt. It is composed of two fold belts and of two overthrusts involving Dabang-Liuma-dawan compressive fold belt, Jianyi-Leji-Qijie overthrust belt, Dianzishang-Qinao fold belt and Bashiyan-Banbi overthrust fault belt.
Keywords:north-westward structure  feature  characteristic  Shazigou area in Zhenling  Guizhou  
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