地震地质 ›› 2007, Vol. 29 ›› Issue (2): 336-353.

• 研究论文 • 上一篇    下一篇

利用磁异常解析方法试验研究城市断裂

张先, 赵丽   

  1. 中国地震局地球物理勘探中心,郑州 450002
  • 收稿日期:2006-09-09 修回日期:2007-03-29 出版日期:2007-06-09 发布日期:2009-08-27
  • 作者简介:张先,男,1945年生,1969年毕业于北京地质学院勘探地球物理系,长期从事利用磁测资料探测震区深部构造及地球动力学方面的研究工作,电话:13598010136,E-mail:dizhenjuzhao@sina.com.
  • 基金资助:
    国家发展与改革委员会发改投资"城市活断层试验探测"项目(20041138)资助

A TEST STUDY OF URBAN FAULTS USING ANALYTICAL METHOD OF MAGNETIC ANOMALY

ZHANG Xian, ZHAO Li   

  1. Geophysical Exploration Center, China Earthquake Administration, Zhengzhou 450002, China
  • Received:2006-09-09 Revised:2007-03-29 Online:2007-06-09 Published:2009-08-27

摘要: 文中选取北京地区作为城市断裂研究试验场,对航磁资料运用解析延拓、功率谱分析、正则化滤波、方向导数、小波分析、分形维数、视磁化强度反演及磁性界面反演等一系列磁异常解析方法进行了数据处理。在处理数据分析与对比研究的基础上,对磁法勘探的各种解释方法在城市断裂研究中所发挥的作用、功效及适应性进行了评估,对今后城市断裂探测研究工作中的磁法勘探技术方面提出了指导性意见。文中对于揭示深部断裂、浅层断裂、基底直立断裂、以及预定方向的断裂和构造两侧磁性差异较大的断裂构造所运用的方法、功效及注意事项均做了较好的说明。另外还对功率谱用于计算不同尺度磁性体场源深度的效果进行了分析。

关键词: 城市断裂, 试验研究, 磁异常解析方法, 北京地区

Abstract: Beijing area is chosen as the testing field to study the urban fault.Aeromagnetic data in the field are processed using analytical methods of magnetic anomaly such as analytical downward continuation,spectrum analysis,regularization filtering,directional derivative,wavelet analysis,fractal dimension,inversion of apparent magnetization and inversion of magnetic surface.The effect,function and adaptability of various interpreting methods of magnetic prospecting are evaluated on the basis of analysis and contrast of a lot of data in the urban fault study.Instructional opinions are proposed about magnetic prospecting techniques in the future urban fault exploration after the test results are summarized.For example,the upward continuation and the regularization filtering or multi-scale separation of wavelets are effective for revealing deep faults.The height of upward continuation and the wavelength of regularization filtering should not be too big,otherwise,it is possible to enhance regional structures and restrain the information of local faults.Downward continuation and vertical derivative are effective for revealing shallow faults.It is necessary to control the largest downward continuation depth to the top of field source,otherwise,the data can not be used because of vibratory results.Horizontal derivative or wavelet analysis of high frequency is effective for revealing faults in the pre-judged direction.Inversion of apparent magnetization is effective for revealing faults in the area where there is a distinct difference of rock magnetism between two sides of the fault.Inversion of base magnetic surface is effective for revealing the vertical basement fault with a big shift of base magnetic surfaces between the two blocks along the fault.In addition,the testing results also show that spectrum analysis has a good effect on computing the field source depth for local anomaly,but not for regional anomaly.We hope that the study results can play an active role in the future exploration of urban faults.

Key words: urban fault, test study, Beijing area, analytical method of magnetic anomaly

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