Geological structure of the Mediterranean Sea floor (based on geological—Geophysical data)

According to geophysical data, the Mediterranean Sea depressions are noted for a peculiar type of the earth's crust. The sedimentary rock sequence is of great thickness (8–15 km) and is of platform-type dislocation. Several structural stages are distinguished in the sedimentary complex. The you...

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Veröffentlicht in:Marine geology 1975-01, Vol.18 (5), p.231-261
Hauptverfasser: Malovitskiy, Ya.P., Emelyanov, E.M., Kazakov, O.V., Moskalenko, V.N., Osipov, G.V., Shimkus, K.M., Chumakov, I.S.
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container_end_page 261
container_issue 5
container_start_page 231
container_title Marine geology
container_volume 18
creator Malovitskiy, Ya.P.
Emelyanov, E.M.
Kazakov, O.V.
Moskalenko, V.N.
Osipov, G.V.
Shimkus, K.M.
Chumakov, I.S.
description According to geophysical data, the Mediterranean Sea depressions are noted for a peculiar type of the earth's crust. The sedimentary rock sequence is of great thickness (8–15 km) and is of platform-type dislocation. Several structural stages are distinguished in the sedimentary complex. The youngest of them are the Messinian (evaporite) and Pliocene—Quaternary stages. The consolidated part of the earth's crust shows small thickness and is divided into large blocks. Vertical dislocations of the large crustal blocks which were conditioned by condensation—rarefaction and the upper mantle substance migration were at the base of Mediterranean sea floor transformation.
doi_str_mv 10.1016/0025-3227(75)90015-8
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title Geological structure of the Mediterranean Sea floor (based on geological—Geophysical data)
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