Aracil Ávila, EnriqueVilas Minondo, Lorenzo2023-06-202023-06-2019870213-683Xhttps://hdl.handle.net/20.500.14352/58130The 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.spajournal articlehttps://sociedadgeologica.org/publicaciones/geogaceta/geogaceta-3-1987/open access551.7JurassicCretaceousFracturationAutomatic-mappingAlbaceteGeología estratigráfica2506.19 Estratigrafía