SEISMIC RISK IN FENNOSCANDIA

被引：23

作者：

BATH, M

机构：

[1] Seismological Institute, Box 417

来源：

TECTONOPHYSICS | 1979年 / 57卷 / 2-4期

关键词：

D O I：

10.1016/0040-1951(79)90152-5

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：

Seismic risk is calculated by means of recurrence periods, obtained from least squares relations between number of earthquakes and magnitude. This method is described and applied to Fennoscandia. The results, summarized in tabular form, give the seismic risk for 54 regions, each comprising 2° in latitude and 2° in longitude, and for the magnitude range from 2.0 to 5.0 on the regional scale. © 1979.

引用

页码：285 / 295

页数：11

共 10 条

[1] SEISMICITY MAP OF SWEDEN [J].

BATH, M .

TECTONOPHYSICS, 1978, 49 (1-2) :T1-T8

[2] ENERGY AND TECTONICS OF FENNOSCANDIAN EARTHQUAKES [J].

BATH, M .

TECTONOPHYSICS, 1978, 50 (01) :T9-T17

[3]

BATH M, 1956, SVER GEOL UNDERS C, V545

[4]

BATH M, SVER GEOL UNDERS

[5]

BATH M, 1976, 576 SEISM I REP

[6]

KULHANEK O, 1976, 876 SEISM I REP

[7]

KULHANEK O, 1978, GEOL MIJNBOUW, V57, P251

[8]

LOMNITZ C, 1976, SEISMIC RISK ENGINEE

[9]

Lomnitz C., 1974, GLOBAL TECTONICS EAR

[10]

SCHEIDEGGER AE, 1975, PHYSICAL ASPECTS NAT

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