Zobrazeno 1 - 10
of 11
pro vyhledávání: '"K. O. Dobrolyubova"'
Autor:
S. G. Skolotnev, A. A. Peyve, A. Sanfilippo, S. Yu. Sokolov, L. Petracchini, K. O. Dobrolyubova, Y. Nestola, A. N. Ivanenko, V. Basch, A. N. Pertsev, C. Sani, Yu. V. Brusilovskiy, C. Ferrando, I. A. Veklich, A. S. Bich, K. N. Sholukhov, A. A. Razumovskii, V. N. Dobrolyubov
Publikováno v:
Oceanology. 62:724-726
Autor:
S. G. Skolotnev, A. A. Peyve, A. N. Ivanenko, K. O. Dobrolyubova, A. Sanfilippo, M. Ligi, S. Yu. Sokolov, I. A. Veklich, L. Petracchini, V. Basch, C. Ferrando, C. Sani, M. Bickert, F. Muccini, C. Palmiotto, M. Cuffaro, D. A. Kuleshov, V. N. Dobrolyubov, N. A. Shkittin, S. A. Dokashenko, E. S. Yakovenko
Publikováno v:
Doklady Earth Sciences. 504:333-337
Publikováno v:
Geotectonics. 56:107-122
Abstract— A retrospective analysis of seismic tomography models with different levels of detail along the Mid-Atlantic Ridge (MAR) has shown that mantle inhomogeneities depicted by variations of seismic waves velocities in low-detail models look la
Publikováno v:
Вестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле, Vol 49, Iss 1, Pp 53-67 (2021)
The thickness of the Atlantic Equatorial segment sedimentary cover decreases with the distance from the continental source of mass removal and increases slightly with the distance from the Mid-Atlantic Ridge (MAR). Background sedimentation makes a sm
Autor:
N. N. Turko, K. O. Dobrolyubova
Publikováno v:
Herald of the Russian Academy of Sciences. 90:395-405
The practice of assigning geographical names to undersea features on the bottom of the World Ocean and standardization of terms and names at the national and international levels are discussed. The development of underwater research technology, an in
Autor:
S. Yu. Sokolov, Yu. A. Zaraiskaya, K. O. Dobrolyubova, E. A. Moroz, N. N. Turko, A. O. Mazarovich, A. S. Abramova
Publikováno v:
Geotectonics. 52:401-420
Manifestations of fluids and deformations in the sedimentary cover, which are both factors of brightening (blanking anomalies) in seismoacoustic records, in the equatorial segment of the Atlantic coincide with the sublatitudinal zones of the activate
Publikováno v:
Geotectonics. 48:175-187
The walls of the Knipovich Ridge are complicated by normal and reverse faults revealed by a high-frequency profilograph. The map of their spatial distribution shows that the faults are grouped into domains a few tens of kilometers in size and are a r
Autor:
Alexander A Peyve, A. A. Razumovskii, A. S. Abramova, Yu. A. Zaraiskaya, K. P. Yampol’skii, A. E. Eskin, K. O. Dobrolyubova, A. A. Chernykh, A. O. Mazarovich, V. N. Efimov, Yu. N. Raznitsyn, N. M. Sushchevskaya, R. Kh. Aliulov, S. G. Skolotnev, A. V. Zaionchek, E. A. Moroz
Publikováno v:
Doklady Earth Sciences. 426:551-555
In 2007, the Geological Institute of the Russian Academy of Sciences (GIN RAS) carried out investigations in the North Atlantic, in the southern part of the Knipovich Ridge extending for 600 km from the Mohns spreading ridge to the Molloy fault zone
Publikováno v:
Russian Journal of Earth Sciences. 3:353-370
Publikováno v:
Russian Journal of Earth Sciences. 3:59-78