科技创新与应用2024，Vol.14Issue(11)：95-98,4.DOI:10.19981/j.CN23-1581/G3.2024.11.022
鄂尔多斯西缘中段断裂体系特征研究
摘要
Abstract
The geological structure of the study area belongs to the Weizhou-Majiatan fold zone in the middle section of the Taole-Pengyang Chong Fault Zone.This special tectonic location and evolution characteristics have created excellent geological conditions for the formation of geothermal and coal resources in this area.Previous studies have shown that fault structures are the most important controlling factor for geothermal and coal deposits.In order to interpret the characteristics of the middle fault system in the western margin of Ordos,based on 1:200 000 regional gravity data,borehole and magnetotelluric sounding profile as constraints,various boundary identification methods such as horizontal derivative and normalized standard deviation are used to finely interpret the fault system in the study area,which provides a basis for later geothermal resources and coal exploration.关键词
鄂尔多斯西缘中段/1∶20万区域重力/边界识别方法/断裂体系/边界识别方法Key words
middle part of the western margin of Ordos/1∶200 000 regional gravity/boundary identification method/fault system/boundary identification method分类
天文与地球科学引用本文复制引用
陈晓晶,虎新军,仵阳,白亚东,曹园园..鄂尔多斯西缘中段断裂体系特征研究[J].科技创新与应用,2024,14(11):95-98,4.基金项目
宁夏自然科学基金项目(2021AAC03451) （2021AAC03451）
宁夏财政专项项目(NXCZ20220206) （NXCZ20220206）
2020年宁夏回族自治区青年拔尖人才培养工程项目(2020079) （2020079）
