SUBDUCTION OF SEDIMENTS AND LEVELS OF 10BE IN LAVAS OF THE KURILE ISLANDS AND KAMCHATKA
- DSpace Home
- →
- Геология России
- →
- ELibrary
- →
- View Item
JavaScript is disabled for your browser. Some features of this site may not work without it.
dc.contributor.author | Tsvetkov A.A. | |
dc.contributor.author | Gladkov N.G. | |
dc.contributor.author | Volynets O.N. | |
dc.date.accessioned | 2020-10-06T05:10:42Z | |
dc.date.available | 2020-10-06T05:10:42Z | |
dc.date.issued | 1989 | |
dc.identifier | https://elibrary.ru/item.asp?id=31089534 | |
dc.identifier.citation | Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1989, , 3, 182-186 | |
dc.identifier.issn | 0891-5571 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/17744 | |
dc.description.abstract | One of the important problems in studying island-arc igneous activity is that of its sources. A key problem is that of demonstrating subduction of an oceanic plate beneath an island arc and the involvement of its component rocks, primary sediments, in island-arc magmatism. The calculations indicate that the highest fraction of sedimentary material in the magma chambers producing present-day lavas of the Kurile volcanoes in less than 4 percent and that for the Kamchatka volcanoes it is less than 2 percent. These results confirm the conclusion that we reached earlier from a study of the isotopic composition of Nd and Sr and the distribution of rare earths, that small but real quantities of sedimentary material were involved in magma generation in the vicinity of the Kurile island arc. Authors data represent the first direct confirmation of the mechanism of subduction in this segment of the Asia-Pacific transition zone and must be borne in mind in geodynamic reconstructions. | |
dc.title | SUBDUCTION OF SEDIMENTS AND LEVELS OF 10BE IN LAVAS OF THE KURILE ISLANDS AND KAMCHATKA | |
dc.type | Статья |
Files in this item
Files | Size | Format | View |
---|---|---|---|
There are no files associated with this item. |
This item appears in the following Collection(s)
-
ELibrary
Метаданные публикаций с сайта https://www.elibrary.ru