CRUSTAL STRUCTURE OF SOUTHWESTERN HONSHU, JAPAN, DERIVED FROM EXPLOSION SEISMIC-WAVES

被引：6

作者：

HASHIZUME, M ^{[1
]}

MATSUI, Y ^{[1
]}

机构：

[1] OKAYAMA UNIV,INST THERMAL SPRING RES,TOTTORI 68202,JAPAN

来源：

GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY | 1979年 / 58卷 / 01期

关键词：

D O I：

10.1111/j.1365-246X.1979.tb01017.x

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

Crustal structure of south‐western Honshu, Japan, has been studied using seismic waves generated by the Kurayosi and Hanabusa explosions. Inversion of the seismic data was first made by Monte Carlo simulation and then for finer revision with the aid of synthetic seismograms. General features of the crustal structure in this area are as follows: the granitic and basaltic layers are sharply separated by the Conrad discontinuity; seismic wave velocity in the basaltic layer increases monotonically to the Moho; and the velocity discontinuity at the Moho, if any, is not distinct. Although lateral inhomogeneity of crustal structure in this area is considered to be large, evidence indicates that the features described above still hold as a major profile of the structure. Copyright © 1979, Wiley Blackwell. All rights reserved

引用

页码：181 / 199

页数：19

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