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Titlebook: Quaternary Period in Saudi Arabia; 1: Sedimentological, Saad S. Al-Sayari (Chairman),Josef Georg Zötl (Pro Book 1978 Springer-Verlag/Wien 1

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Saad S. Al-Sayari (Chairman),Josef Georg Zötl (Pro
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Acknowledgementspecial thanks go to H. E. Dr. ., Rector of the University of Petroleum and Minerals in Dhahran, and to Professor Dr. ., President of the Austrian Academy of Sciences. The team also wishes to thank Professor Dr. E. ., Vice-President of the Austrian Academy of Sciences, and the members of the Academy,
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Geologyn to rifting in the Red Sea, separation of Arabia and Africa, continental drift, sea floor spreading, and plate tectonics. It has been of interest also for the part it appears to have played in the folding and elevation of the Zagros Mountains in western Iran and the Oman Mountains during the Alpine
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Climatert), except for parts of North and South Yemen, the ’Asir province of Saudi Arabia, and northeastern Oman (Fig. 3), where the temperatures are lower, the rainfall is greater than in the remaining part of the peninsula, and where the vegetation consists of mountain forest and woodland.
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Ar Rub’ Al Khaliy which characteristics of the Quaternary in general can be inferred. Additional evidence for earlier phases of the Quaternary must be derived from correlation with similar sediments in surrounding areas, from the Tertiary tectonic history of the Arabian plate, and from other more indirect lines of
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