| 注册
首页|期刊导航|地质力学学报|重磁电综合地球物理探测河套盆地深部结构

重磁电综合地球物理探测河套盆地深部结构

刘嵘 马见青 李庆春 叶培盛

地质力学学报2016,Vol.22Issue(4):943-954,12.
地质力学学报2016,Vol.22Issue(4):943-954,12.

重磁电综合地球物理探测河套盆地深部结构

GRAVITY, MAGNETIC AND ELECTRIC COMPREHENSIVE GEOPHYSICAL PROSPECTING FOR DEEP STRUCTURES IN HETAO BASIN

刘嵘 1马见青 1李庆春 1叶培盛2

作者信息

  • 1. 长安大学地质工程与测绘学院,西安710054
  • 2. 中国地质科学院地质力学研究所,北京100081
  • 折叠

摘要

Abstract

The gravity,magnetic,and electrical methods have been used to reveal the structure developed in the deep covered area of the Hetao Basin.We have carried out a lot of research on the characteristics of the northern and southern boundary faults,the features and thickness of Quaternary sediments and the structures developed in the basement of the Hetao Basin.A preliminary study on the distribution of Quaternary aquifer in this area was made by using electrical resistivity method.The joint inversion results of gravity and magnetic data,and earthquake data have been analyzed.And four concealed fault F1 to F4 from south to north and Langshan-Seertengshan piedmont fault F5 have been revealed.The fluctuation and buried depth of the crystalline basement in the area have been revealed.Depth of the basement in the southern part of the study area is about 2.5 ~4.2 km,and which in the northern part is up to 6 km.North Adjacent to the Seertengshan piedmont fault,the basement rock has been uplifted to about 0-1 km.

关键词

河套盆地/磁法勘探/重力勘探/超高密度电法/结晶基底/隐伏断层

Key words

Hetao Basin/magnetic prospecting/gravity exploration/ultrahigh density resistivity method/crystalline basement/buried fault

分类

天文与地球科学

引用本文复制引用

刘嵘,马见青,李庆春,叶培盛..重磁电综合地球物理探测河套盆地深部结构[J].地质力学学报,2016,22(4):943-954,12.

基金项目

中国地质调查局地质调查项目“特殊地质地貌区填图试点”(DD20160060) (DD20160060)

国家自然科学基金项目(41374145) (41374145)

中国地质调查局特殊景观区填图试点项目(12120114042101) (12120114042101)

长安大学中央高校基本科研业务费专项资金项目(2013G1261060) (2013G1261060)

地质力学学报

OA北大核心CSCDCSTPCD

1006-6616

访问量0
|
下载量0
段落导航相关论文