长江断裂带安徽段上地壳速度结构及基底特征  

COMPREHENSIVE INTERPRETATION OF THE UPPER CRUSTAL VELOCITY STRUCTURE AND CRYSTALLINE BASEMENT OF THE CENTRAL YANGTZE FAULT ZONE FROM AIR-GUN SOURCE DATA

作　　者：邓晓果 田晓峰[1] 杨卓欣[1] 王夫运[1] 刘宝峰[1] 高占永 郑成龙[1] DENG Xico-guo;TIUN Xico-feno;YANG Zhuo-xin;WANG Fu-yuo;LIU Bco-feno;GAO Zhay-gppo;ZHENG Cheno-loua(Geophysical Exploration Center of CEA,Zhengzhou 450003,China)

机构地区：[1]中国地震局地球物理勘探中心,郑州450003

出　　处：《地震地质》2020年第5期1109-1128,共20页Seismology and Geology

基　　金：国家重点研发计划项目(2018YFC1503200);国家自然科学基金(41674068,41790463,41774071)共同资助。

摘　　要：长江断裂带是中国东部构造体制转换的典型地区,具有断隆相间、“一盖多底”的构造特征,发育了大量金属矿区,精细的上地壳速度结构和基底图像对该区的成矿作用和构造演化研究具有较为重要的意义。文中以在长江航道内激发的大容量气枪作为震源获得的密集观测数据为基础,综合利用初至波走时成像、时间项和射线反演等方法,构建了长江断裂带安庆—马鞍山段的上地壳精细速度结构和基底结构。综合分析研究结果可知,长江断裂带的上地壳精细速度结构和结晶基底特征显示该区具有断隆相间的构造特征。怀宁盆地是该段上地壳最厚的区域,其基底埋深约4.5km。庐枞盆地的结晶基底埋深约为4.1km,沉积盖层呈明显的坳陷盆地形态,结晶基底及其下方存在相对高速的速度特征。长江断裂带在跨江处的上地壳存在明显的速度横向变化,显示了长江断裂带切断基底的断裂特征。长江断裂带安徽段基底最浅的区域为铜陵隆起区,埋深仅为2.2km,表明铜陵隆起区新生代以来经历了强烈的挤压作用。The Yangtze fault zone is a typical tectonic regime transition zone of the eastern China.Tectonically,it is characterized by alternated rifts and uplifts and“several crystalline basements with one sediment cover”.Abundant metal metallogenic deposits are developed.Improvement of the velocity model and basement structure will benefit our understanding and knowledge about the regional tectonics.Large volume airgun sources have been broadly applied to seismic surveys due to significant advantages.For instance,they are environmentally friendly,use lower frequencies,and are repea-table.Several seismic and geological research institutions,such as China Earthquake Admi-nistra-tion,carried out a three-dimensional comprehensive sounding using the large volume airgun as the seismic source which was fired at the channel of the Yangtze River in 2015.The source-receiver geometry of this seismic experiment covered the whole Anhui Province which locates at the Middle-Lower Yangtze River.The densest observational area is in the Middle-Lower Yangtze River Metallogenic Belt which is a narrow area along the Yangtze River and consists of the Luzong,Tongling,Ningwu,and Anqing-Guichi ore deposits.The Tanlu fault zone,a giant strike-slip fault of more than 2-000km long,passes through the northwestern margin of this area.Geophysical studies have demonstrated copious geological evidences for the Yangtze fault zone,which is appro-ximately 450km long and crosses central China,extending to the eastern coastal area.The present fault and fold systems are the consequences of the repeated tectonic events since the Mesozoic.We collected and analyzed the seismic data of 20 fixed airgun shot points,then utilized tomography,time term method and head wave traveltime inversion based on ray tracing techniques to model the upper crustal velocity and crystalline basement structure of the Anqing-Maanshan segment beneath the Yangtze fault zone.The profile along the Yangtze River consists of 100 PDS-2 seismometers with a spacing of 2km.We applied the li

关 键 词：长江断裂带 大容量气枪 上地壳速度结构 结晶基底 

分 类 号：P315.2[天文地球—地震学]