The up-lift is one of active karst control factor. However, examples of inactive preterits structures in the
east coast of Majorca Island could be direct relation with up-lift and fracturation. Regionally, post-Miocene
up-lift have not influenced in the paleocollapase structures genesis because the sinking was controlled by
the lithology. Therefore, analysing 1304 fractures in the Santanyí carbonate platform these show three
great groups with different genesis and chronology. One group shows a dominant direction toward NOSE.
The second group is orientated to NE-SO. And the last one is lineated to E-O and N-S, may be related
with genesis of paleocollapase