SOURCE PARAMETERS OF RECENT STRONG EARTHQUAKES IN NORTHEASTERN IRAN FROM LONG-PERIOD SURFACE-WAVES

被引：0

作者：

NIAZI, M ^{[1
]}

KANAMORI, H ^{[1
]}

机构：

[1] CALTECH,SEISMOL LAB,PASADENA,CA 91125

来源：

TECTONOPHYSICS | 1983年 / 93卷 / 3-4期

关键词：

D O I：

10.1016/0040-1951(83)90277-9

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：205 / 205

页数：1

共 50 条

[1] SOURCE PARAMETERS OF 1978 TABAS AND 1979 QAINAT, IRAN, EARTHQUAKES FROM LONG-PERIOD SURFACE-WAVES
NIAZI, M
KANAMORI, H
[J]. BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, 1981, 71 (04) : 1201 - 1213
[2] SOURCE PHASE AND AMPLITUDE ANOMALIES OF LONG-PERIOD SURFACE-WAVES
UM, JH
DAHLEN, FA
[J]. GEOPHYSICAL RESEARCH LETTERS, 1992, 19 (15) : 1575 - 1578
[3] EXTRACTION OF LONG-PERIOD SURFACE-WAVES
LANE, SS
[J]. TRANSACTIONS-AMERICAN GEOPHYSICAL UNION, 1978, 59 (04): : 319 - 319
[4] USE OF LONG-PERIOD SURFACE-WAVES FOR RAPID-DETERMINATION OF EARTHQUAKE-SOURCE PARAMETERS
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GIVEN, JW
[J]. PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 1981, 27 (01) : 8 - 31
[5] MEASURING COMPLEX SPECTRA OF LONG-PERIOD SURFACE-WAVES FOR EARTHQUAKE SOURCE ANALYSIS
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LAY, T
[J]. GEOPHYSICAL RESEARCH LETTERS, 1989, 16 (03) : 259 - 262
[6] LONG-PERIOD SURFACE-WAVES AND MANTLE BOUNDARY UNDULATIONS
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[J]. GEOPHYSICAL JOURNAL INTERNATIONAL, 1994, 116 (01) : 205 - 216
[7] LONG-PERIOD SURFACE-WAVES OF FOUR WESTERN UNITED-STATES EARTHQUAKES RECORDED BY THE PASADENA STRAINMETER
DOSER, DI
KANAMORI, H
[J]. BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, 1987, 77 (01) : 236 - 243
[8] SOURCE FINITENESS OF LARGE EARTHQUAKES MEASURED FROM LONG-PERIOD RAYLEIGH-WAVES
ZHANG, JJ
KANAMORI, H
[J]. PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 1988, 52 (1-2) : 56 - 84
[9] MANTLE ANISOTROPY BENEATH THE TIBETAN PLATEAU - EVIDENCE FROM LONG-PERIOD SURFACE-WAVES
YU, Y
PARK, J
WU, F
[J]. PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 1995, 87 (3-4) : 231 - 246
[10] PROGRESS REPORT ON THE DETERMINATION OF SEISMIC MOMENT TENSOR FROM LONG-PERIOD SURFACE-WAVES
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[J]. TECTONOPHYSICS, 1982, 84 (01) : 1 - 2

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