摘要
为了深入研究三峡重庆库区岩石圈动力学特征及其对断裂构造活动的控制和影响,并为之提供基础资料,为三峡重庆库区地震、地质灾害的监测与防治提供基础依据,在已有地球物理资料的基础上,从综合地球物理研究角度出发,通过实测地震测线资料的再解释,采用新的处理技术方法,对本区的东西向主剖面和南北向支测线的地震测深资料进行二维射线追踪处理、Pg波成像;选用场分离技术、位移数字成像技术重新处理了重力和航磁资料,通过联合反演来建立深部二维构造剖面,对剖面所揭示的基底构造特征和地壳结构特征、主要断裂构造特征以及莫霍面的起伏特征进行了精细分析和细致研究,从地球物理平面场特征出发建立了岩石圈构造三维框架。研究结果表明,这样的研究思路准确、方法得当,结论可靠;沿该剖面,把可解译的断裂分为Ⅲ级:Ⅰ级为超岩石圈断裂;Ⅱ级为壳断裂;Ⅲ级为盖层断裂。依据地球物理特征,准确揭示了库区的断裂构造特征,达到了预期效果。
For the purpose of providing fundamental data to study the lithosphere dynamic characteristics and the controlling or influence on rupture activity, monitoring and preventing the geological disaster and earthquake, this paper processes the practical seismic data includeing west-east and north-south sections. Selects separating field and displacing digital imaging to process the gravity and magnetic data, analyzes the earth＇s crust structure and main rupture as well as Moho fluctuating. The 2-D structure section was achieved through joint inversion. The results indicate that the strategy is appropriate and the results are reliable. Along the main section. The interpretable rupture can be classified into three suits, first class （ Ⅰ ） is super lithosphere rupture that cuts deeply to up mantal, second class （ Ⅱ ） is lithosphere rupture that exists in the Earth crust, third class （Ⅲ） is rupture in covering layer （including fundus rupture）. According to geophysical features. The rupture structure characteristics can be accurately got, and the results agree with the real situation quite well.
出处
《地球科学与环境学报》
CAS
2005年第3期49-54,共6页
Journal of Earth Sciences and Environment
基金
国家科技攻关计划项目(2001B091A37)
关键词
构造特征
地震
重力
航磁
射线追踪
平面场
断裂
三峡
长江
重庆库区
construct character
seism
gravity
magnetism
ray tracing
plane field
rupture
Yangtze Gorges
Yangtze River
Chongqing Reservoir area
作者简介
胡建平（1958-），男．陕西子洲人，天津城市建设学院教授，西安交通大学博士研究生，从事计算机科学与技术和地球物理综合研究。
