Abstract
All cruises of Ukrainian recearch vessels usually begin in the Black and Mediterranean seas. Consequently the Branch of Geology of Oceans and Seas of the Institute of Geological Sciences of the National Academy of Sciences, which is the oldest marine geology scientific centre of Ukraine, have a considerable data base and map archive On the ground of marine geological data obtained in many routes in the Black and Mediterranean seas we have realized the comparative studying of sedimentation processes within the Black Sea and the Levantine Basin of Eastern Mediterranean. Certain results obtained are discussed in this paper. Geochemical aspects of sediment accumulation in the Black and Levantine seas were considered in detail in [1, 2, 3].
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References
Babinetz A. E., Mitropolsky A. Y., Olshtynsky, S. P. (1973) Hydrogeological and Geochemical Peculiarities of Deep Sea Sediments of the Black sea, Naukova Dumka, Kiev. (Russian).
Emelyanov E. M., Mitropolsky A. Y., Shimkus, K. M, Moussa, A. A. (1979) Ceochemistry of the Mediterranean Sea, Naukova Dumka, Kiev. (Russian).
Mitropolsky A. Y., Bezborodov A. A., Ovsyany, E. I. (1982) Geochemistry of the Black Sea, NaukovaDumka, Kiev. (Russian).
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© 1999 Springer Science+Business Media Dordrecht
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Mitropolsky, A.Y., Olshtynsky, S.P. (1999). Comparative analysis of sedimentation processes within the Black Sea and Eastern Mediterranean. In: Malanotte-Rizzoli, P., Eremeev, V.N. (eds) The Eastern Mediterranean as a Laboratory Basin for the Assessment of Contrasting Ecosystems. NATO Science Series, vol 51. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-4796-5_18
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DOI: https://doi.org/10.1007/978-94-011-4796-5_18
Publisher Name: Springer, Dordrecht
Print ISBN: 978-0-7923-5586-1
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