Zobrazeno 1 - 4
of 4
pro vyhledávání: '"N. I. Dykan"'
Autor:
N. I. Dykan, L. A. Viskova, Sergey V. Popov, I. A. Goncharova, I. A. Nikolaeva, Tatiana N. Pinchuk, T. M. Kozyrenko, Larisa A. Golovina, Yu. V. Vernyhorova, A. V. Koromyslova, N. Yu. Fillippova, Yu. V. Rostovtseva, L. B. Iljina, Eleonora P. Radionova
Publikováno v:
Paleontological Journal. 50:1039-1206
The Taman sections, reference for the Neogene of the Eastern Paratethys, are investigated thoroughly paleontologically and stratigraphically, with level-by-level description of four sections, correlated in detail with each other; fossil remains comin
Autor:
V. V. Rudjuk, A. I. Krokhmal, S. K. Prylypko, N. I. Dykan, M. S. Komar, T. F. Khrystoforova, V. N. Shelkoplyas
Publikováno v:
Geological Journal. :7-25
The analysis of the history of the construction of stratigraphic schemes of the Quaternary deposits inUkraineis given over the past 40 years. The scheme of Department of the Geotectonic and the Quaternary Geology of the IGS of AS USSR (1969), the sch
Autor:
N. I. Dykan
Publikováno v:
Geological Journal; № 1 (2012); ст. 57-66
Геологический журнал; № 1 (2012); ст. 57-66
Геологічний журнал; № 1 (2012); ст. 57-66
Геологический журнал; № 1 (2012); ст. 57-66
Геологічний журнал; № 1 (2012); ст. 57-66
Some aspects of the historical development of ostracodes of Euxinian basin in Middle Miocene-Pliocene are specified. There are ostracodes migratory connections between Paratethys basins (Euxinian, Pannonian, Dacic) and Mediterranean basin; he recurre
Autor:
N. I. Dykan
Publikováno v:
Geological Journal; № 3 (2011); ст. 29-38
Геологический журнал; № 3 (2011); ст. 29-38
Геологічний журнал; № 3 (2011); ст. 29-38
Геологический журнал; № 3 (2011); ст. 29-38
Геологічний журнал; № 3 (2011); ст. 29-38
At the first the local biostratigraphic subdivisions according to ostracoses (Complex-Zone, Eco-Zone, Acme-Zone, layers of ostracodes) were separated in the Middle Miocene-Pliocene deposits of the TamanskyPeninsula (key-sections "capePopovStone", "ca