Age and conditions of formation of sedimentary cover of the Ulleung Plateau of the Sea of Japan according to micropaleontological data

Author:

Tsoy I. B.,Gorovaya M. T.,Vasilenko L. N.,Vashchenkova N. G.,Vagina N. K.

Publisher

Pleiades Publishing Ltd

Subject

Paleontology,Stratigraphy,Geology

Reference67 articles.

1. Baldauf, J.G. and Barron, J.A., Evolution of biosiliceous sedimentation patterns—Eocene through Quaternary: paleoceanographic response to polar cooling, in Geological History of the Polar Oceans: Arctic Versus Antarctic, Netherlands: Kluwer Acad. Publ., 1990, pp. 575–607.

2. Bathymetric Chart (1: 500000) of the Middle Part of East Sea, no. B4623, The Korea Hydrogr. Oceanogr. Admin., Ministry of Oceans and Fisheries, Republic of Korea, 2013.

3. Baturin, G.N. and Derkachev A.N., Phosphate inclusions in tuffites from the Krishtofovich Rise (Sea of Japan), Oceanology, 2007, vol. 47, no. 5, pp. 730–740.

4. Bersenev, I.I., Bersenev, Yu.I., Lelikov, E.P., et al., New data on the geological structure of Japan Sea floor (R/V Pervenetz, Cruise 20), in Geologiya okrainnykh morei Tikhogo okeana (Geology of Marginal Seas of the Pacific Ocean), Vladivostok: Far Eastern Sci. Center Akad. Nauk SSSR, 1975, pp. 3–14.

5. Bersenev, I.I., Lelikov, E.P., Bezverkhnii, V.L., et al., Geologiya dna Yaponskogo morya (Geology of the Japan Sea Floor), Vladivostok: Far Eastern Sci. Center Akad. Nauk SSSR, 1987 [in Russian].

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