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凭祥-东门大断裂中段特征及控岩控相初析--以宁明-板利地区为例
引用本文:蒙有言,周秋娥,李玉坤.凭祥-东门大断裂中段特征及控岩控相初析--以宁明-板利地区为例[J].南方国土资源,2002,15(4):1-4.
作者姓名:蒙有言  周秋娥  李玉坤
作者单位:1. 中国地质大学地球科学院,湖北,武汉,430074
2. 广西区域地质调查研究院,广西,桂林,541003
摘    要:文章收集了凭祥-东门大断裂在宁明-板利地区的详细资料,研究该断裂在该地区的表现特征,分析其活动性质及期次,阐明了该大断裂具有多期次活动的特点,并且在不同期次和不同地段具有不同的活动特点和表现形式,在此基础上结合区域地层、岩石特征,阐明其对区域的控岩、控相作用,为三级构造单元界线的划分提供了基础资料.

关 键 词:特征    控岩    控相    凭祥-东门大断裂    宁明-板利
文章编号:1003-7861(2002)04-0001-04
修稿时间:2002年4月17日

THE CHARACTERISTICS AND CONTROLLING SEDIMENTARY FACIES AND GRANITOID ANALYSIS OF THE MIDDLE PART OF PINGXING-DONGMENG LARGE FAULT--An Example of Ningming-Banli Regions
Authors:MENG You-yan  ZHOU Qiu-e  LI Yu-kun
Institution:MENG You-yan 1,ZHOU Qiu-e 2,LI Yu-kun 2
Abstract:This article mainly studies characteristics of Pingxing-Dongmeng large fault in Ningming-Banli regions by collecting the plenty and detail materials of the fault, and analyses its features of activities and periods of activities. The study shows that the fault had the characteristics of multiple-periods of activities and different activities in different periods and regions, it is proved that the fault controlled depositional-environment and distribution of rock in this region. The studies will offer new fundamental information for the research of boundary of third order structural element.
Keywords:characteristics  controlling granitoid  controlling sedimentary facies  Pingxing-Dongmeng large fault  Ningming-Banli  
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