MANIFESTATION OF EARLY PALEOZOIC MAGMATISM IN THE SOUTH YENISEI RIDGE
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dc.contributor.author | Vernikovskaya A.E. | |
dc.contributor.author | Vernikovsky V.A. | |
dc.contributor.author | Yasenev A.M. | |
dc.contributor.author | Datsenko V.M. | |
dc.contributor.author | Sal'nikova E.B. | |
dc.contributor.author | Kovach V.P. | |
dc.contributor.author | Kotov A.B. | |
dc.contributor.author | Travin A.V. | |
dc.date.accessioned | 2022-07-18T05:29:18Z | |
dc.date.available | 2022-07-18T05:29:18Z | |
dc.date.issued | 2004 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=13454411 | |
dc.identifier.citation | Doklady Earth Sciences, 2004, 397, 6, 747-752 | |
dc.identifier.issn | 1028-334X | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/38270 | |
dc.description.abstract | U-Pb- and Ar-Ar-geochronologic data are presented, obtained for Posolnenskii and Nizhnekanskii massifs located in the central and south-western parts of Angaro-Kanskii block and breaking through the metamorphic rocks of Enisei and Kan series. As established, granitoids of Posolnenskii and Nizhnekanskii massifs were formed in the Late Cambrian-Middle Ordovician periods in the range from 510 to 455 ma. These data allow considering their formation as a reflection of Early Caledonian collision-accretion events widely manifested in the Central-Asian folded belt. | |
dc.subject | Ordovician | |
dc.title | MANIFESTATION OF EARLY PALEOZOIC MAGMATISM IN THE SOUTH YENISEI RIDGE | |
dc.type | Статья | |
dc.subject.age | Paleozoic::Ordovician | |
dc.subject.age | Палеозой::Ордовикская | ru |
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