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The formation of the fractures of the Tablate area (situated in the transition between the Granada basin and the Alpujarran corridor) was controlled by the progressive and important uplift of Sierra Nevada, occurred from the late Miocene. Consequently, the direction of the extension is close to that occurred at the South of Sierra Nevada and the characteristics of the paleostress ellipsoid are congruent with this uplift. On the other hand, two local controls have been observed in the development of the minor fractures: there is a clear lithologic influence, particularly in the contact between levels of silts and other formed by coarser sediments. Moreover, local changes of the stress produced a different grade of the fracturation.  La formación de las fracturas del área de Tablate (situada en el tránsito de la cuenca de Granada al corredor de las Alpujarras) fue controlada por el levantamiento de Sierra Nevada ocurrido a partir del Mioceno superior. En consecuencia, la dirección de extensión se acerca a la que se produjo al sur de Sierra Nevada y las características de los elipsoides de paleoesfuerzos son congruentes con el levantamiento. Por otra parte, existen dos controles locales en el desarrollo de las fracturas menores: hay una neta influencia de la litología, particularmente en el paso de niveles formados por sedimentos detríticos finos a otros gruesos y, además, cambios locales del esfuerzo producen un diferente grado de fracturación

Fracture controls in Tablate (Lecrín, Granada, Betic Chain, Spain)