Faults in the study area are dip-slip normal faults.
Deep-seated faults in this work have complex lateral and vertical segmentation.
The deep-seated faults were reactivated in Late Jurassic, Early Cretaceous and Paleocene.
Fluid-related anomalies show close link with the deep-seated faults.
Hydrocarbons were leaked through faults during fault reactivation.
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