SOFT-SEDIMENT DEFORMATION IN THE QUATERNARY SEDIMENTS OF THE LOWER MAHI RIVER BASIN, WESTERN INDIA

摘要

A variety of soft-sediment deformation structures are documented in the Lower Mahi river basin of Western India. They are slumps and slides, syn-tectonic folds, faulting, slickensides and pseudonodules. Majority of the structures indicate syn-tectonic sedimentation and differential subsidence of the basin. The movements took place along several step faults developed parallel to the East Cambay Basin Margin Fault. [References: 15]