ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
鄂尔多斯盆地北部重磁场及其基底断裂特征研究
  
关键词:cratonization and reactivation  structural framework  basement fault  basement gravity and magnetic anomaly fields  northern Ordos Basin
基金项目:国家自然科学基金项目(编号: 41172127; 41572102);陕西省煤田地质集团科技管理部项目(编号: SMDZ-2022ZD-5; SMDZ-2023ZD-09)
作者单位E-mail
田刚 陕西省煤田地质集团有限公司
自然资源部煤炭资源勘查与综合利用重点实验室
陕西省煤田物探测绘有限公司
西北大学地质系 
691561570@qq.com 
汶小岗 自然资源部煤炭资源勘查与综合利用重点实验室
陕西省煤田物探测绘有限公司 
 
薛海军 自然资源部煤炭资源勘查与综合利用重点实验室
陕西省煤田物探测绘有限公司 
 
马丽 陕西省煤田地质集团有限公司
自然资源部煤炭资源勘查与综合利用重点实验室 
 
蒲仁海 西北大学地质系  
宋立军 西安石油大学地球科学与工程学院  
陈杰 中国石油大学(北京)地球科学学院  
陈硕 陕西省煤田地质集团有限公司
自然资源部煤炭资源勘查与综合利用重点实验室
陕西省煤田物探测绘有限公司
西北大学地质系 
 
吴大林 陕西省煤田物探测绘有限公司  
杨明慧 中国石油大学(北京)地球科学学院  
摘要点击次数: 1267
全文下载次数: 657
摘要:
Study on Gravity and Magnetic Fields and Characteristics of Basement Faults in the Northern Ordos Basin
      To elucidate the characteristics of basement faults in the northern Ordos Basin, an analysis of its gravity and magnetic field characteristics was conducted. Wavelet multiscale decomposition and power spectrum analysis methods were used to comprehensively identify and interpret the obtained basement gravity and magnetic anomaly fields. The results reveal that the Bouguer Gravity anomaly field in the northern Ordos Basin exhibited higher values in the east and lower values in the west. Simultaneously, the aeromagnetic field was organized into zones of nearly east–west (EW) positive and negative. A total of 28 intra-basin basement faults were identified in the northern Ordos Basin, with north–east (NE) and EW trending basement faults being predominant, and NW and SN trending faults distributed in a staggered or oblique tectonic framework; The EW–NE basement fault originated from the continental collision event between the ~1.95 Ga Yinshan Block and the Ordos Block. The Xinzhao North–Porjianghaizi South (F4+F10) basement fault zone serves as a boundary of different tectonic units before the Mesoproterozoic. Moreover, The SN–NW trending faults are a tearing structure formed during the continental collision process, selectively activated in the EW-trending tensile stress field in the Mesoproterozoic. The formation of the basement fault system in the northern Ordos Basin is attributed to the interaction between different continents and is selectively activated in later stages. This evidence of structural deformation contributes valuable insights into the study of the North China cratonization and reactivation process.
Tian Gang,Wen Xiaogang,Xue Haijun,MA Li,PU Renhai,Song Lijun,Chen Jie,Chen Shuo,WU Dalin,Yang Minghui.2024.Study on Gravity and Magnetic Fields and Characteristics of Basement Faults in the Northern Ordos Basin[J].Acta Geoscientica Sinica,45(3):279-290.
查看全文  查看/发表评论  下载PDF阅读器
Copyright©2008 All Rights Reserved
Sponsored by:
Address:: PostCode: Tel: E-mail: