太要断裂东段覆盖区地球物理特征及推断解释

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英文篇名：Geophysical Characteristics of Loess-covered Area in the Eastern Segment of Taiyao Fault,Xiaoqinling Mountains 作者：田庆水 ; 王孟霞 ; 郑燕 ; 倪云鹏 ; 豆猛 ; 常勤慧 英文作者：TIAN Qingshui;WANG Mengxia;ZHENG Yan;NI Yunpeng;DOU Meng;CHANG Qinhui;Henan Aero Geophysical Survey and Remote Sensing Center;Solid Mineral Geophysical Exploration Engineering Technology Research Center of Henan Province;Geological Survey Institute of Henan Province; 关键词：太要断裂 ; 覆盖区 ; 地球物理特征 ; 小秦岭 英文关键词：Taiyao fault;;loess coverage area;;geophysical characteristics;;Xiaoqinling 中文刊名：西北地质 英文刊名：Northwestern Geology 机构：河南省航空物探遥感中心;河南省固体矿产地球物理探测工程技术研究中心;河南省地质调查院; 出版日期：2019-09-05 出版单位：西北地质 年：2019 期：03 基金：河南省两权价款地质勘查项目“河南省小秦岭北麓覆盖区金矿预查”(2011-93);; 河南省两权价款地质科研项目“河南省小秦岭北麓隐伏区物探找金技术研究”(2011-622-12)资助 语种：中文; 页：257-268 页数：12 CN：61-1149/P ISSN：1009-6248 分类号：P631

摘要

通过对小秦岭北麓黄土覆盖区重力测量、音频大地电磁测深(AMT)、可控源音频大地电磁测深(CSAMT)、二维地震等物探勘查资料进行分析、处理和综合研究,总结了太要断裂东段的深部特征和分布形态。研究认为:太要断裂东段沿小秦岭北麓近东西向呈波状展布,断裂具有分枝复合现象,主断层处在盆地内黄土覆盖区;断裂为高角度正断层,倾角为65°～80°,总断距在3 000m左右;断裂错断了中、新生界和太华群内的韧性剪切带,对矿体具有破坏作用;太要断裂主要发育期始于中生代晚白垩世以后,晚于小秦岭变质核杂岩的拆离断层发育形成时间。
        After carrying out the gravity survey,Audio Magnetotelluric sounding(AMT),Controlled Source Audio-frequency Magnetotelluric sounding(CSAMT),2 Dseismic survey in the loess covered area of the north Xiaoqinling Mountains,the related data has been analyzed,processed and comprehensively studied in this paper.And then,the deep fracture characteristics and distribution pattern of eastern segment of Taiyao fault have been summarized.The result shows that the eastern segment of Taiyao fault extends in near EW direction,showing wavy distribution along the north Xiaoqinling Mountains and having the phenomenon of separation and reunion.The main fault is located in the loess covered area of the basin,which belongs to the high-angle normal fault,with the inclination of 65°-80°and the total fault displacement of about 3000 m.This fault dislocates the Mesozoic and Cenozoic strata,as well as the ductile shear zone in the Taihua Group,which destroys the gold deposit.The Taiyao fault was mainly developed after late Cretaceous,which is later than the formation of detachment fault of metamorphic core complex in Xiaoqinling Mountains.

引文

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