COMPARISON BETWEEN DEFORMATION DEDUCED FROM ANALYSIS OF RECENT FAULTS AND FROM FOCAL MECHANISMS OF EARTHQUAKES (AN EXAMPLE - PAPHOS REGION, CYPRUS)

被引：21

作者：

MERCIER, J

VERGELY, P

DELIBASSIS, N

机构：

[1] UNIV PARIS S, CTR SCI, LAB GEOL DYNAM, ORSAY, FRANCE

[2] NATL OBSERV ATHENS, SEISMOL INST, ATHENS, GREECE

来源：

TECTONOPHYSICS | 1973年 / 19卷 / 04期

关键词：

D O I：

10.1016/0040-1951(73)90026-7

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：315 / 332

页数：18

共 15 条

[1]

Arthaud F., 1969, B SOC GEOL FR, V7, P729

[2]

AUBOUIN J, 1971, GEOL RUNDSCH, V60, P833

[3] COMPUTER DETERMINATIONS FOR FAULT-PLANE SOLUTIONS IN AND NEAR ANATOLIA [J].

CANITEZ, N ;

UCER, B .

TECTONOPHYSICS, 1967, 4 (03) :235-&

[4]

CONSTANTINESCU L, 1965, STUDII CERCETARI G G, V3, P173

[5] PLATE TECTONICS AND GEOSYNCLINES [J].

DEWEY, JF ;

BIRD, JM .

TECTONOPHYSICS, 1970, 10 (5-6) :625-&

[6]

Galanopoulos A., 1965, PRAKT AKAD ATHENON, V40, P387

[7]

HOGSON JH, 1956, ANN GEOL PAYS HELL, V8, P29

[8] RIDGES AND BASINS OF TONGA-KERMADEC ISLAND ARC SYSTEM [J].

KARIG, DE .

JOURNAL OF GEOPHYSICAL RESEARCH, 1970, 75 (02) :239-+

[9]

LOWE KE, 1946, AM MINERAL, V31, P425

[10] PACIFIC-TYPE OROGENY AND ITS MODEL-EXTENSION OF PAIRED BELTS CONCEPT AND POSSIBLE ORIGIN OF MARGINAL SEAS [J].

MATSUDA, T .

TECTONOPHYSICS, 1971, 11 (01) :5-&

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