岷江—雪山梁子断裂带的时空构架及其演化特征研究  

The research of time and space frame and evolution of Minjiang Xueshan Liangzi fault

作　　者：康波[1] 赵玉鹏 熊丽媛[1] 

机构地区：[1]四川省核工业地质调查院,四川成都610061 [2]四川省地矿局区域地质调查院,四川成都610213

出　　处：《内蒙古石油化工》2015年第3期134-136,共3页Inner Mongolia Petrochemical Industry

摘　　要：岷江—雪山梁子断裂带的大地构造位置位于扬子大陆北缘与华北大陆南缘的结合部,地质背景十分复杂。此区域内以前地质工作者及专门研究此问题的研究人员对岷江—雪山梁子断裂带的认识存在很多分歧,本文通过分析研究对其时空格架及演化特征提出一些自己的认识。Minjiang Xueshan Liangzi fault is located in the junction of the northern margin of the Yangtze continental mainland and southern edge of North China where the geological background is very complicated.Geologists and specialized researchers who explore this problem of Minjiang Xueshan Liangzi fault have different understandings.This paper analyses the time and space frame and the evolution of fault and proposes some own understandings about it.

关 键 词：断裂带 时空构架 物质组成 断裂特征 演化特征 地震活动 

分 类 号：P618.130.2[天文地球—矿床学]