Climatic, eustatic, and tectonic controls on Quaternary deposits and landforms, Red Sea Coast, Egypt

Author:

Arvidson Raymond,Becker Richard,Shanabrook Amy,Luo Wei,Sturchio Neil,Sultan Mohamed,Lotfy Zakaria,Mahmood Abdel Moneim,El Alfy Zeinhom

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference33 articles.

1. Abdou , N. Y. Some geomorphic features of the coastal plain of the Red Sea, south of Gulf of Suez, Egypt Cairo, Egypt 1991

2. Distribution of some planktonic foraminifera species in deep-sea cores from the Red Sea and their relation to eustatic sea level changes;Behairy;Palaeogeo. Paleoclimatol. Paleoecol.,1984

3. Quaternary sea level fluctuations on a tectonic coast: New 230Th/234U dates from the Huon Peninsula, New Guinea;Bloom;Quat. Res.,1974

4. Small scale convection induced by passive rifting: The cause of uplift of rift shoulders;Buck;Earth Planet. Sci. Lett.,1986

5. Late Pleistocene beaches and wadi alluvia near Marsa Alam, Red Sea Coast, Egypt;Butzer;Paleoecol. Afr. Surround. Isl. Antarct. Capetown,1976

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