3-DIMENSIONAL ATTENUATION STRUCTURE BENEATH NORTH ISLAND, NEW-ZEALAND

被引：23

作者：

SATAKE, K ^{[1
]}

HASHIDA, T ^{[1
]}

机构：

[1] UNIV TOKYO,EARTHQUAKE RES INST,BUNKYO KU,TOKYO 113,JAPAN

来源：

TECTONOPHYSICS | 1989年 / 159卷 / 3-4期

关键词：

D O I：

10.1016/0040-1951(89)90127-3

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：181 / 194

页数：14

共 23 条

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[3]

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[4] DETERMINATION OF 3-DIMENSIONAL VELOCITY ANOMALIES UNDER A SEISMIC ARRAY USING 1ST-P ARRIVAL TIMES FROM LOCAL EARTHQUAKES .1. A HOMOGENEOUS INITIAL MODEL [J].

AKI, K ;

LEE, WHK .

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[5]

EIBY GA, 1977, B NZ NAT SOC EARTHQU, V10, P167

[6]

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[7]

Gutenberg B., 1956, B SEISMOL SOC AM, V46, P105, DOI [10.1785/bssa0460020105, DOI 10.1785/BSSA0460020105, 10.1785/BSSA0460020105]

[8]

HAINES AJ, 1981, B SEISMOL SOC AM, V71, P275

[9] SEISMIC-WAVE VELOCITIES IN THE UPPERMOST MANTLE BENEATH NEW-ZEALAND [J].

HAINES, AJ .

NEW ZEALAND JOURNAL OF GEOLOGY AND GEOPHYSICS, 1979, 22 (02) :245-257

[10] THICKNESS OF MANTLE SEISMIC ZONE BENEATH NORTH ISLAND OF NEW ZEALAND [J].

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GALE, AW .

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