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Almost all the sites drilled in the Arabian Sea (Table 1, Figure 1) sampled sediments representing most of Cenozoic time. Thus, it is possible to discuss the results of this part of Leg 23 of the Deep Sea Drilling Project in terms of the development of a normal ocean basin formed largely by, and subject to, processes of sea floor spreading. The Red Sea sites on the other hand (Table 2, Figure 1) sampled only the last 5 m.y. of the geological record, and the results from these cores pertain to the rather special processes (evaporite formation, initiation of oceanic crust) associated with the break-up of continental crust by sea floor spreading. Therefore, in making comparisons between the sites drilled on Leg 23, the discussion is divided into two sections treating the Arabian Sea and Red Sea sites separately.

Summary of General Features of Arabian Sea and Red Sea Cenzoic History Based on Leg 23 Cores