DIFFERENTIAL PCP TRAVEL TIMES AND RADIUS OF CORE

被引：26

作者：

ENGDAHL, ER

JOHNSON, LE

机构：

[1] UNIV COLORADO,COOPERAT INST RES ENVIRONM SCI,BOULDER,CO 80302

[2] UNIV CALIF,DEPT GEOL & GEOPHYS,SEISMOG STN,BERKELEY,CA 94720

来源：

GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY | 1974年 / 39卷 / 03期

关键词：

D O I：

10.1111/j.1365-246X.1974.tb05466.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：

引用

页码：435 / 456

页数：22

共 41 条

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[2] RESOLVING POWER OF GROSS EARTH DATA
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[3] BACKUS G, 1971, AM MATH SOC LECT APP, V14, P1
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[5] Berzon I. S., 1972, IZV AN USSR PHYS EAR, V6, P21
[6] CHARACTER OF MANTLE-CORE BOUNDARY FROM OBSERVATIONS OF PCP WAVES
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[J]. EARTH AND PLANETARY SCIENCE LETTERS, 1972, 16 (02) : 166 - +
[7] PDP AND PKIKP WAVES AND DIFFRACTED PCP WAVES
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[J]. GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1970, 20 (04): : 367 - &
[8] BUCHBINDER GG, 1973, B SEISMOL SOC AM, V63, P2047
[9] BUCHBINDER GG, 1968, B SEISMOL SOC AM, V58, P1797
[10] PROPERTIES OF CORE-MANTLE BOUNDARY AND OBSERVATIONS OF PCP
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