用Pg波走时重建华北地区结晶基底速度及时间项图像  

RECONSTRUCTION OF THE BASEMENT VELOCITIES AND TIME-TERMS USING Pg WAVES IN NORTH CHINA REGION

作　　者：宋占隆[1] 杨卓欣[1] 石金虎 张先康[1] 李松林[1] 杨健[1] 

机构地区：[1]国家地震局地球物理勘探中心,郑州450003

出　　处：《华北地震科学》1997年第2期9-16,共8页North China Earthquake Sciences

基　　金：地震科学联合基金

摘　　要：应用层析成象反投影方法，对华北地区28条深地震测深剖面Pg波走时进行处理，作出了该区结晶基底速度及时间项成象。并作了方法的数值模型合成数据的敏感性分析，证明所采用方法的有效性及成象结果的可靠性。计算中应用LSQR算法求解大型稀疏超定方程。并采用只存储矩阵非零元素技术，使存储量减小到原矩阵的百分之一，同时零元素不参加计算，提高了运算速度。华北地区结晶基底速度为5.9～6.35km／s，时间项最大为2.0s。The crystal basement velocities and time-terms in North China region are imaged by a tomographic backprojection using Pg waves from 28 pro filles. Quantitative analyses of the algorithms are given by synthetic data of the digital model. The results from the test show that our method is quite stable and reliable. The LSQR algorithm is used for solving overdetermined equations. The zero elements of the large sparse matrix are not stored and calculated. Thus the store amount is reduced to one percent. The speed of calculation is raised greatly. The minimum and maximum velocities are 5. 9km/s and 6. 35km/s respectively. The maximum time-term is 2.0 second.

关 键 词：地震勘探 地震波 地震测深 结晶基底 CT 

分 类 号：P631.4[天文地球—地质矿产勘探] P548.2[天文地球—地质学]