V.Ye. Ivanov, I.E. Lomakin
Department of Marine Geology and Sedimentary Ore Formation, National Academy of Sciences of Ukraine, Kyiv
GEOLOGICAL POSITION AND TECTONICS OF THE LOMONOSOV PALEOVOLCANIC MASSIFF AND FOROSS LEDGE
The significant differences in geological history, tectonic and volcanism of individual sections of Continental margins is founded in zone, previously has been isolated as paleoisland arc in the north part of the Black Sea. Large blocks of the continental slope are devided by the deep faults, which are an extension of naturally oriented disjunctive network in south Ukraine.
Key words: Lomonosov bloks, Phoros bloks, lineament, magma action, neotectonic.
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