RT Journal Article
T1 Estructuración del basamento mesozoicoen Los Llanos de Albacete
A1 Aracil Ávila, Enrique
A1 Vilas Minondo, Lorenzo
AB The Mesozoic basement of Los llanos de Albacete Tertiary Basin shows a fracture grid with two main orientations, almost orthogonal: NE-SW orientation is preferential, causing the basement to be divided in severa/ blocks, limited by lystric faults and divided in smaller 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 several wells. Aracil, E. y Vilas, L. (1987): Estructuración del basamento mesozoico en Los Llanos de Albacete. Geogaceta, 3, 19-22.
PB Sociedad Geológica de España
SN 0213-683X
YR 1987
FD 1987
LK https://hdl.handle.net/20.500.14352/58130
UL https://hdl.handle.net/20.500.14352/58130
LA spa
DS Docta Complutense
RD 12 abr 2025