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This document summarizes a geological study of the Dera Ghazi Khan city area in Pakistan. It finds that while the area lies near the folded Zinda Pir anticline, no active faults are found directly beneath the city. Regional studies within 100 km2 found several active faults up to 70-75 km from the city capable of magnitude 5-7 earthquakes. Detailed studies within 25 km2 of the city found no evidence of recent ground movement in alluvial or talus deposits. Therefore, the document concludes that Dera Ghazi Kh

Author

mustafa

Language

EN