DEEP-STRUCTURE OF THE VANUATU (NEW-HEBRIDES) ISLAND-ARC - INTERMEDIATE DEPTH COLLISION OF SUBDUCTED LITHOSPHERIC PLATES

被引：15

作者：

HANUS, V ^{[1
]}

VANEK, J ^{[1
]}

机构：

[1] CZECHOSLOVAK ACAD SCI, INST GEOTECH & GEOPHYS, S-14131 PRAGUE, CZECHOSLOVAKIA

来源：

NEW ZEALAND JOURNAL OF GEOLOGY AND GEOPHYSICS | 1983年 / 26卷 / 02期

关键词：

D O I：

10.1080/00288306.1983.10422513

中图分类号：

P5 [地质学];

学科分类号：

0709 ; 081803 ;

摘要：

引用

页码：133 / 154

页数：22

共 26 条

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[7] MORPHOLOGY OF THE WADATI-BENIOFF ZONE, ANDESITIC VOLCANISM, AND ACTIVE FRACTURE-ZONES IN CENTRAL-AMERICA [J].

HANUS, V ;

VANEK, J .

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[8] MORPHOLOGY OF ANDEAN WADATI-BENIOFF ZONE, ANDESITIC VOLCANISM, AND TECTONIC FEATURES OF NAZCA PLATE [J].

HANUS, V ;

VANEK, J .

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[9] PLATE TECTONIC INTERPRETATION OF DEEP EARTHQUAKES BETWEEN THE TONGA-LAU AND NEW-HEBRIDES SUBDUCTION ZONES [J].

HANUS, V ;

VANEK, J .

TECTONOPHYSICS, 1981, 75 (3-4) :T19-T28

[10] GEODYNAMIC INTERPRETATION OF THE EARTHQUAKE DISTRIBUTION IN THE KERMADEC SUBDUCTION ZONE [J].

HANUS, V ;

VANEK, J .

STUDIA GEOPHYSICA ET GEODAETICA, 1978, 22 (03) :259-275

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