Zobrazeno 1 - 8
of 8
pro vyhledávání: '"T. E. Sedysheva"'
Publikováno v:
Oceanology. 62:879-889
Publikováno v:
Oceanology. 61:1026-1039
Publikováno v:
Russian Journal of Pacific Geology. 14:460-471
Based on a detailed bathymetric map of the southeastern part of the Magellan Seamounts created using the results of multibeam echo sounding, a lineament analysis of the seafloor relief was performed, linear landforms were distinguished and their azim
Publikováno v:
Russian Journal of Pacific Geology. 10:435-442
Analysis of detailed bathymetric charts and records of phototelevision profiling over the surfaces of the guyots of the Magellan Seamounts reveals many cones and domes. Their diameters and heights vary from a few hundreds of meters to 10 km and from
Publikováno v:
Lithology and Mineral Resources. 51:1-12
Buried ferromanganese nodules and their stratiform accumulations (nodule horizons), which are widespread in sedimentary sequences of the Magellan Seamounts, have been studied in core obtained by shallow drilling on its guyots in the course of expedit
Publikováno v:
Russian Journal of Pacific Geology. 6:217-229
The geological-prospecting investigations carried out by scientists from the Yuzhmorgeologiya State Scientific Center in the eastern segment of the Magellan Seamounts of the Pacific during the cruise of the R/V Gelendzhik in 2003–2010 brought new d
Publikováno v:
Russian Journal of Pacific Geology. 3:401-410
The geological-geophysical studies carried out in the western part of the Pacific Ocean by the State Research Center “Yuzhmorgeologiya“ during cruises of the R/V “Gelendzhik” in 2002–2004 yielded new data on the relief of the Gramberg Guyot
Autor:
I. A. Basov, Yu. D. Zakharov, V. D. Khudik, T. E. Sedysheva, S. P. Pletnev, M. E. Mel’nikov, T. A. Punina
Publikováno v:
Russian Journal of Pacific Geology. 1:257-264
New materials obtained in the Pacific during cruises of the R/V Gelendzhik carried out by the State Scientific Center Yuzhmorgeologiya in 2000–2001 make it possible to specify the geologic and geomorphologic structure of Alba Guyot and clarify lith