Part of seismic profile 122-23 (Indus Fan). Shown is a basement ridge, which we interpret to be of Mesozoic age and of continental origin.

Part of seismic profile 122-23 (Indus Fan). Interpretation shows a basement ridge which exhibit stratified sediments on top (red) which are truncated before sedimentation of drift sediments (below unconformity bMM, darker grey). Onlap termination hints to a Mesozoic age (pre-rift) and a continental origin of the ridge. The onset of channnel-complex above bMM unconformity is clearly visible.

Quelle: BGR