The connection has been distorted by a sinistral shear fault, which has displaced the point of connection by ~ 350 km.
2.
Four types of traps have been identified in offshore Indus : an extensional rollover anticline trend in the upper slope, drape structures over the Eocene carbonate banks and seamounts, stratigraphic traps formed by sands pinching out against the Murray Ridge and folds associated with the Murray Ridge shear faults and shale diapirs.
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