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《Geology in China》 2007-01
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Processing method of deep seismic reflection data from the basin-range junction zone on the northeastern margin of the Qinghai-Tibet Plateau and preliminary geological understanding

WANG Hai-yan1,GAO Rui1,MA Yong-sheng2,ZHU Xuan2,LI Qiu-sheng1,LI Peng-wu1,KUANG Zhao-yang1,3,LU Zhan-wu1(1.Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China;2.Southern Exploration & Production Company,Sinopec,Kunming 650021,Yunnan,China;3.No.6 Geophysical Prospecting Party,East China Petroleum Administration,Sinopec,Nanjing 210007,Jiangxi,China)  
The basin-range junction zone has complex surface geological conditions and a rather undulate tomography,where deep seismic reflection data are characterized by a low S/N ratio,strong multifold noises and great lateral variation in velocity.According to the characteristics of these deep seismic reflection data,the authors used the ProMAX processing system to make refraction static correction,pre-stack noise attenuation,surface consistent processing,man-machine interactive velocity analysis,residual static correction circulating iterative processing,NMO based on surface and post-stack noise suppression on the 2-D deep seismic reflection data(or called the Spo4-2 profile) across the junction zone of the Zoigê basin and West Qinling orogen and found a set of processing method and flow process suited to the low S/N ratio deep reflection data of the basin-range junction zone.Finally they got the SP04-2 stacked section.The section for the first time reveals the lithospheric structure of the basin-range junction zone of the Zoigê basin and West Qinling orogen and offer a reliable seismologic basis for studying the contact relationships in the deep interior of the basin-range zone.
【Fund】: 国家自然科学基金重点项目(40334035);; 青年科学基金项目(40604010)
【CateGory Index】: P631.4
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