Implicaciones neotectónicas de la serie sísmica de Adra (1993-1994)Ejemplo de un terremoto compuesto.
-
1
Universidad Complutense de Madrid
info
ISSN: 0213-683X
Argitalpen urtea: 1996
Zenbakien izenburua: Comunicaciones presentadas en el IV Congreso Nacional de Geología, Alcalá de Henares, 1996
Zenbakia: 20
Orrialdeak: 834-837
Mota: Artikulua
Beste argitalpen batzuk: Geogaceta
Laburpena
In this work has been analysed the 1993-1994 Adra seismic sequence characterized by two mainshocks of magnilude 5.0 and 4.9. The local neotectonic, aftershock distribution and fault plane solutions are performed and we find significant relations between them this seismic sequence respond to a "compound earthquake mechanism" caused by the reactivation of a N 170 E fault (second mainshock mb: 4.9) as a result of the first mainshock (mb: 5.0) asociated to a N 135 E oblique slip fault. The aflershock activity is acumulated into a fault bounded crustal block as a result of the field stress readjustment and changes in the pore pressure triggered off by the two mainshocks.