Seismotectonics of Portugal and its adjacent Atlantic area

被引:109
作者
Borges, JF
Fitas, AJS
Bezzeghoud, M
Teves-Costa, P
机构
[1] Univ Evora, Dept Fis, P-7002552 Evora, Portugal
[2] Ctr Geofis Evora, P-7002552 Evora, Portugal
[3] Univ Lisbon, Ctr Geofis, Lisbon, Portugal
[4] Univ Lisbon, FCUL, Lisbon, Portugal
[5] Univ Lisbon, Dept Fis, Lisbon, Portugal
关键词
seismicity; focal mechanisms; stress indicator; Portugal; seismotectonics;
D O I
10.1016/S0040-1951(00)00291-2
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
A study of focal mechanisms of earthquakes and stress indicators are presented for Portugal and its adjacent Atlantic margins. Recently Riberio et al. (1996) published a work on this subject. In this study, we introduce new focal mechanisms of nine earthquakes. We use these results together with 12 other focal mechanisms and the main tectonic features in the region to define more accurately the type of mechanism and the stress pattern of the region. All the focal mechanisms used in this study differ partially but are compatible with the regional stress held. The stress indicators resulting from focal mechanisms and other geological and geophysical data show that the Portugal continental and its Atlantic margins are under horizontal pressure in NNW-SSE direction, with a greater proportion of strike-slip and reverse-oblique mechanisms for the whole area. (C) 2001 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:373 / 387
页数:15
相关论文
共 28 条
[1]   CLOSURE OF THE AFRICA EURASIA NORTH AMERICA PLATE MOTION CIRCUIT AND TECTONICS OF THE GLORIA FAULT [J].
ARGUS, DF ;
GORDON, RG ;
DEMETS, C ;
STEIN, S .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1989, 94 (B5) :5585-5602
[2]   Constrains on the source of the 1755 Lisbon tsunami inferred from numerical modelling of historical data on the source of the 1755 Lisbon tsunami [J].
Baptista, MA ;
Miranda, PMA ;
Miranda, JM ;
Victor, LM .
JOURNAL OF GEODYNAMICS, 1998, 25 (1-2) :159-174
[3]  
Bezzeghoud M, 1999, B SEISMOL SOC AM, V89, P359
[4]  
BORGES J, 1999, P WORKSH WEB US AN U, P31
[5]  
BORGES JF, 1991, METODOS AUTOMATICOS, P93
[6]  
BRILLINGER DR, 1980, B SEISMOL SOC AM, V70, P149
[7]   SEISMICITY, SOURCE MECHANISMS AND TECTONICS OF THE AZORES-GIBRALTAR PLATE BOUNDARY [J].
BUFORN, E ;
UDIAS, A ;
COLOMBAS, MA .
TECTONOPHYSICS, 1988, 152 (1-2) :89-118
[8]  
BUFORN E, 1988, REV GEOFIS, V44, P109
[9]   TRIANGLE DIAGRAMS - TERNARY GRAPHS TO DISPLAY SIMILARITY AND DIVERSITY OF EARTHQUAKE FOCAL MECHANISMS [J].
FROHLICH, C .
PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 1992, 75 (1-3) :193-198
[10]   ISOSEISMAL MAP OF THE 1755 LISBON EARTHQUAKE OBTAINED FROM SPANISH DATA [J].
MARTINEZSOLARES, JM ;
LOPEZARROYO, A ;
MEZCUA, J .
TECTONOPHYSICS, 1979, 53 (3-4) :301-313