Geological structure of the submarine Vityaz Ridge within the Seismic Gap area (Pacific slope of the Kurile island arc)
作者： E. P. Lelikov , I. B. Tsoy , T. A. Emel’yanova , E. P. Terekhov , N. G. Vashchenkova
DOI: 10.1134/S1819714008020012
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摘要: Results of geological research conducted by the Pacific Oceanological Institute Far East Division Russian Academy Sciences and Oceanology on submarine Vityaz Ridge during Cruise 37 R/V Akademik M.A. Lavrentyev in 2005 are discussed. Various rocks constituting basement sedimentary cover ridge were dredged three areas ridge. Based isotope geochronology, petrogeochemical, petrographic, paleontological data comparison with similar available from adjacent land Sea Okhotsk, they subdivided into several age complexes. Late Cretaceous, Eocene, Oligocene, Miocene, Pliocene-Pleistocene complexes defined among igneous rocks, while volcanogenic-sedimentary united Cretaceous-Early Paleocene (late Campanian-Danian), undivided Paleogene (Paleocene-Eocene?), Oligocene-early The obtained formation settings made it possible to reconstruct evolution central slope Kurile island arc.
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