• Corpus ID: 131525732

KOMEX (Kurile Okhotsk Sea Marine Experiment). Cruise reports KOMEX V and VI: RV Professor Gagarinsky Cruise 26 and MV Marshal Gelovany Cruise 1

@inproceedings{Biebow2000KOMEXO,
  title={KOMEX (Kurile Okhotsk Sea Marine Experiment). Cruise reports KOMEX V and VI: RV Professor Gagarinsky Cruise 26 and MV Marshal Gelovany Cruise 1},
  author={Nicole Biebow and Thomas L{\"u}dmann and Boris Ya. Karp and R. G. Kulinich},
  year={2000}
}
Mineral composition of tephra layers in the Quaternary deposits of the Sea of Okhotsk:: Heavy minerals associations and their geochemistry
Heavy mineral associations from tephra layers in the Quaternary deposits of the Sea of Okhotsk and their chemical characteristics were studied by various techniques. It was shown that such
On the age of the sedimentary cover of the Kurile Basin, Sea of Okhotsk
A velocity model of the upper Earth’s crust of the Kurile Basin, Sea of Okhotsk, is constructed using experimental seismic data. Four layers are distinguished in the sedimentary cover with the
Crustal and Mantle Structure of the Sea of Okhotsk, Pacific Northwest: A Review
The deep structure of the Sea of Okhotsk under seismically dangerous regions is studied. The main feature of the deep structure in the region is the occurrence of an asthenospheric layer in the upper
Ancient subduction zone in Sakhalin Island
Abstract The northern part of Sakhalin Island is an area of recent intensive tectonic movements and hydrothermal processes, as well as a place of accumulation of useful minerals. The deep structure
Changes of planktonic and benthic foraminiferal assemblages in upper quaternary sediments of the Deryugin Basin, Sea of Okhotsk
The analysis of foraminiferal assemblages in sediments that were deposited during the last 30 kyr revealed similar patterns in their distribution in the central and marginal parts of the Deryugin
Geochemical characteristics of the surface layer of bottom sediments from the Deryugin Basin, Sea of Okhotsk
This paper reports data, including new analyses, on the contents of Ni, Co, V, Mo, Fe, Mn, Zn, Ba, Sc, Y, Cd, Rb, Cs, and W in the sediments of the Deryugin Basin. The features of the distribution of
Millennial-Scale Changes of Intermediate Water Ventilation, Productivity and Nutrient Supply in the Okhotsk Sea and Subarctic North Pacific During the Last 18,000 Years
The modern North Pacific plays a critical role in marine biogeochemical cycles, as it is today the largest natural oceanic sink of CO2 and harbors some of the most biologically productive and least
Neotectonics of the Deryugin Basin area (Sea of Okhotsk)
AbstractThe data of the bottom “summit” surface were used for compiling the schematic structural-neotectonic map and map of the main neotectonic structural elements. Their comparison with the
Foraminifers in late Pleistocene-Holocene sediments of the Deryugin Basin of the Sea of Okhotsk
The study of foraminifers from sediments accumulated during the last 30 ky revealed their similar distribution in the central and marginal parts of the Deryugin Basin, which implies similar
Methane Hydrates and Plumes in the Sea of Okhotsk
Methane hydrates exist beneath the sea bottom near cold seeps NE off the Sakhalin in the Sea of Okhotsk. Multidisciplinary field operations were performed at a study area (approximately 16 × 20 km2)
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