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The sedimentary sequence in the Kuril Islands
International Geology Review, 1976Geological surveys and shallow drillings indicate that a thick series of normal marine sedimentary rocks, lying below the Miocene-Pliocene and Quaternary volcanics on all the islands of the Greater Kuril arc, shows prospects for oil and gas.
A.A. Trofimuk +7 more
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The birds of the Kuril Islands
Proceedings of the United States National Museum, 1898USNM_index ...
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Landscape diversity of the Kuril Islands
Geography and Natural Resources, 2012We consider the use of two approaches in assessing landscape diversity of a territory: qualitative and quantitative analyses of the landscape structure on the basis of landscape maps, and a space imagery-based calculation of landscape diversity. This study revealed that the two approaches under consideration reflect different properties of landscape ...
K. S. Ganzei, A. N. Ivanov
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Soil macrofauna of the south of Kunashir Island (Kuril Islands, Russia)
Doklady Biological Sciences, 2014Study of the soil biota organization under the con ditions of minimal human influence in different soil types is one of the most important tasks for both fun damental and applied soil biology. When developing the concept of the zoological method of soil diagnos tics, Gilyarov [6] considered the taxonomic diversity and the number of species of the ...
K B, Gongalsky +4 more
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Volcanoes of the Kurile Islands
1970Our main task was the study of the volcanoes of the Kurile arc, and to their description we have devoted most of our attention. In all, 160 Quaternary terrestrial volcanoes and volcanic groups are described in the present work, i.e., twice as many as in our earlier summaries. Of these, 104 volcanic edifices have been active in the Holocene.
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Tin potential of the Kuril Islands
International Geology Review, 1973(1973). Tin potential of the Kuril Islands. International Geology Review: Vol. 15, No. 7, pp. 781-783.
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The Sea of Okhotsk—Kuril Islands Ridge and Kuril—Kamchatka Trench
1985The area discussed in this chapter shows a considerable degree of heterogeneity. The northern and central parts of the Sea of Okhotsk form part of an epi-Mesozoic platform built up of deformed geosynclinal rocks ranging in age from Precambrian to Cretaceous covered by only slightly deformed Upper Paleogene and Neogene rocks (Fig. 1).
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