Estructuración del basamento mesozoico en Los Llanos de Albacete
- 1 Instituto de Geología Económica. CSIC-UCM Facultad de Ciencias Geológicas.Madrid.
ISSN: 0213-683X
Argitalpen urtea: 1987
Zenbakia: 3
Orrialdeak: 19-22
Mota: Artikulua
Beste argitalpen batzuk: Geogaceta
Laburpena
The Mesozoic basement of Los llanos de Albacete Tertiary Basin shows a fracture grid with two main orientations, a/most orthogonal: NE-SW orientation is preferential, causing the basement to be divided in severa/ blocks, limited by lystric faults and divided in sma- 1/er structures tilted to the NE. The Neogene filling of the basin is not affected by these faults. The results have been obtained during the study of severa/ wells.