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引用本文:赵成彬,刘保金,酆少英,姬计法,李春周.«��̨���ѵ���ά�ṹ����[J].大地测量与地球动力学,2013,33(6):41-44.
作者姓名:赵成彬  刘保金  酆少英  姬计法  李春周
摘    要:??о???????????????????????????????????????μ?????????????????????????????????550 m×875 m????????????????????????????????????????????????????????????????N20°??22°E????????????и???????????????F1????SE???ζ???F2????NW?????????????????F1????????ζ???F2?£???????ζ???F2???F1?????????????????????????????????????????????????????F??1??F??2??????????????????????????????????????????????????????С??????????780??800 mF2????鲢??F1???????

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THREE DIMENSION STRUCTURE OF LUHUATAI FAULT
Abstract:In order to investigate geometry shape and activity of Luhuatai Fault Zone which locates in the northwest Yinchuan Basin??a 3D seismic exploration was completed whin an area of 550 m×875 m.The results show that it is a buried active fault zone and consisted of two faults??main fault F??1 and secondary fault F??2.The fault zone moved untill the late stage of Middle Pleistocene. Trend of F??1 is SE??and F??2 is NW??both of them are normal faults. The activity time of F??1 is newer than that of F??2??and the fault throw of F??1 is larger than that of F??2. The buried deepth of the up??breakpoint of F??1 has a trend of increasing from North to South. The distance between F??1 and F??2 increases gradually from North to South on the horisontal plane??reduces gradually with depth increase on the vertical profile??and F??2 merges into F??1 at the depth of about
780-800 m.
Keywords:3D seismic technique  buried active fault  DMO correction  coherent data analysis  visualization technology  
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