Resumen de Estructuración del basamento mesozoico en Los Llanos de Albacete

Lorenzo Vilas Minondo, Enrique Aracil Ávila

• 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.