TIME-TERM ANALYSES OF EXPLOSION SEISMIC DATA

TIME-TERM ANALYSES OF EXPLOSION SEISMIC DATA
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爆炸地震数据的时程分析

DOI:
10.4294/jpe1952.20.47
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发表时间:
1972
期刊:
Journal of physics of the earth
影响因子:
--
通讯作者:
S. Asano
S. Asano
中科院分区:
--
文献类型:
--
作者:
T. Yoshii;S. Asano

文献摘要

被引文献

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利用时间项方法对两个地区的爆破地震资料进行了研究。松代震群区两条地震剖面的结果与ASANO等人的模型吻合得很好。在一条地震剖面中,走时残差的纵坐标与横坐标的距离呈凸形趋势,强烈地表明了基底层中存在垂直速度梯度。修正的时间项方法可以准确地确定与距离相关的速度。本研究中使用时间项方法获得的模型消除了HASHIZUME等人气仙沼-大贺剖面模型中的一些缺陷。特别值得注意的是,在本州-日本海边界附近的Pn速度的横向变化的可能性被指出。
Explosion seismic data in two regions are studied by utilizing the time-term method. The results of two profiles in the Matsushiro earthquake swarm area agree very well with the previous models by ASANO et al. In one profile, the travel-time residuals plotted in the ordinate to distances in the abscissa show a convex tendency which strongly suggests vertical velocity gradient in the basement layer. The distance-dependent velocity is determined accurately with the modified time-term method.Some defects in the model by HASHIZUME et al. for the Kesennuma-Oga profile are removed by the model obtained with the time-term method in the present study. It is particularly remarkable that the possibility of the lateral change in the Pn velocity near the Honshu-Japan Sea boundary is pointed out.