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Olistostromal beds and extensive slumping structures were observed.
In the middle Andaman, U5 contains Recent sediment deposition, which is partly associated with westward dipping slumping structures (Fig. 6).
The chaotic and semitransparent nature of reflection patterns (Stoker et al. 1991) seen in the upper part of U5 agrees with the presence of westward dipping slumping structures.
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The sandstone bed is of Ta, Tb and Tc turbidite Bouma horizons and shows slumped structures associated with the appearance of large foraminifera, as well as patch-reef carbonates.
Such features as colour, ripple marks, mud cracks, raindrop imprints, and slump structures are directly observable in the field.
The marine distributary channels include cross bedding as shown in Fig. 4a, lenticular bedding, parallel bedding as shown in Fig. 4b, blocky bedding, and slump structures.
Deposits of such turbidity currents (turbidites) are typified by normal and reverse graded bedding, occasional crude cross bedding, and slump deformation structures.
Core observations also reveal plant stem carbon dust, boulder clay, and slump deformation structures along with sedimentary structures such as low-angle oblique bedding, trough cross bedding, and parallel bedding (Fig. 7).
The occurrence of slump-related structures as observed in the Middle Andaman region (Fig. 6), to the east of the AFB, indicates that slope failures must have occurred due to the high gradient.
Even at Triton's low surface temperature, nitrogen or methane ice is not strong enough to support structures of that height without slumping.
Kawamoto took this to heart and immediately set about not only reviving a slumping corporate giant but radically transforming its management structure.
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