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At fault margins, the rate of sediment supply exceeded accommodation space.
It is thickest near the central part of the southeastern normal fault margins, suggesting development of a large alluvial fan near a transfer zone.
SP I at the base consists of mouth-bar to delta-front and volcaniclastic deposits, and shows rapid facies variations along the southeastern normal fault margins.
The alluvial fan depositional systems, with mainly southwest and southeast source supplies, entered the lakes quickly to form fan deltas; multisource fan deltas were interconnected to form fan delta aprons distributed along the fault margins (Wang et al. 2012).
Notably, the cumulative thickness of SP III to SP V is thickest near the northeastern and southwestern strike-slip margins, suggesting migration of the loci of maximum subsidence from the normal fault margins towards the strike-slip margins after deposition of SP II.
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The western coastal margin is defined by the NW SE trending marginal fault; northern margin is controlled by the North Kathiawar fault.
This means that it shows its everyday action in the form of aseismic creep, the slow, steady sliding of land along the fault's margin.
The major fault systems East Margin Fault (EMF), Western Andaman Fault (WAF) and Diligent Fault (DF) in the AFB, are imaged on the seismic sections (Figs. 4, 6, 7).
Design margins, fault protection and containment were considered as three good approaches to solve safety issue.
The model suggested by the authors pointed out that normal faults bound the margins of these basins and indicate that such a configuration forming at a step-over between two strike-slip fault segments requires subsidence and localized crustal stretching that can be responsible for structural evolution of deep basins in the Marmara Sea (Örgülü 2011).
This has been reported earlier for numerous faults and continental margins (e.g., Brune [1968]; Voisin et al. [2004]; Mulargia et al. [2004]).
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