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EFFECT OF A VELOCITY GRADIENT AT BASE OF MANTLE ON DIFFRACTED P WAVES IN SHADOW

被引：31
作者：
PHINNEY, RA
ALEXANDE.SS
机构：
来源：
JOURNAL OF GEOPHYSICAL RESEARCH | 1969年 / 74卷 / 20期
关键词：
D O I：
10.1029/JB074i020p04967
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
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页码：4967 / &
相关论文
共 8 条
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[3]   ANALYSIS OF AMPLITUDES OF SHORT-PERIOD P WAVES RECORDED BY LONG RANGE SEISMIC MEASUREMENTS STATIONS IN DISTANCE RANGE 30 DEGREES TO 102 DEGREES [J].
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[4]   SEISMIC EVIDENCE FOR A NEW LAYERED STRUCTURE OF EARTHS CORE [J].
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[6]  
HALES AL, 1968, B SEISMOL SOC AM, V58, P1975
[7]   DIFFRACTION OF P BY CORE - A STUDY OF LONG-PERIOD AMPLITUDES NEAR EDGE OF SHADOW [J].
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CATHLES, LM .
JOURNAL OF GEOPHYSICAL RESEARCH, 1969, 74 (06) :1556-&
[8]   P WAVE DIFFRACTION THEORY AND STRUCTURE OF CORE-MANTLE BOUNDARY [J].
PHINNEY, RA ;
ALEXANDE.SS .
JOURNAL OF GEOPHYSICAL RESEARCH, 1966, 71 (24) :5959-+
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