GEOCHRONOLOGY, GEOCHEMISTRY, AND GEODYNAMIC SETTING OF PALEOZOIC GRANITOIDS IN THE EASTERN SEGMENT OF MONGOL-OKHOTSK BELT
- 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 | Sorokin A.A. | |
dc.contributor.author | Sorokin A.P. | |
dc.contributor.author | Kudryashov N.M. | |
dc.contributor.author | Rublev A.G. | |
dc.contributor.author | Levchenkov O.A. | |
dc.contributor.author | Kotov A.B. | |
dc.contributor.author | Sal'nikova E.B. | |
dc.contributor.author | Kovach V.P. | |
dc.date.accessioned | 2022-01-15T07:43:06Z | |
dc.date.available | 2022-01-15T07:43:06Z | |
dc.date.issued | 2003 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=13440482 | |
dc.identifier.citation | Doklady Earth Sciences, 2003, 393, 8, 1136-1140 | |
dc.identifier.issn | 1028-334X | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/34324 | |
dc.description.abstract | Investigated is a series of granitoid massifs in the composition of Yankansky, Tukuringrskii, Jagdinsky, Seledjino-Kerbinsky, Tokursky terrenes. The results of U-Pb-geochronologic, geochemical and Sm-Nd-isotope-geochemical analyses imply that eastern segment of the Mongolian-Okhotsk fold belt contains granitoid complexes of wide age range: from Early to Late Paleozoic period. The obtained data enable to concretize substantially the history of Mongolian-Okhotsk fold belt. | |
dc.subject | Paleozoic | |
dc.title | GEOCHRONOLOGY, GEOCHEMISTRY, AND GEODYNAMIC SETTING OF PALEOZOIC GRANITOIDS IN THE EASTERN SEGMENT OF MONGOL-OKHOTSK BELT | |
dc.type | Статья | |
dc.subject.age | Paleozoic | |
dc.subject.age | Палеозой | ru |
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