EARLY PALEOZOIC GRANITOID BATHOLITHS OF THE ALTAI-SAYAN FOLDED REGION (LATERAL-TEMPORAL ZONING AND SOURCES)
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dc.contributor.author | Rudnev S.N. | |
dc.contributor.author | Vladimirov A.G. | |
dc.contributor.author | Kruk N.N. | |
dc.contributor.author | Ponomarchuck V.A. | |
dc.contributor.author | Babin G.A. | |
dc.contributor.author | Borisov S.M. | |
dc.date.accessioned | 2022-07-25T04:36:28Z | |
dc.date.available | 2022-07-25T04:36:28Z | |
dc.date.issued | 2004 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=13463081 | |
dc.identifier.citation | Doklady Earth Sciences, 2004, 396, 4, 492-495 | |
dc.identifier.issn | 1028-334X | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/38408 | |
dc.description.abstract | This communication discusses the issue of the formation of Early Caledonian batholiths based on comparative analysis of their age and Nd-Isotope characteristics in thee Altai-Kuznetsk -Batenev segment dominated by collisions of the arc-seamount type and the Tuva-Mongolia segment dominated by collisions related to the amalgramation of a synonymous microcontinent and the Tannuol are. We have analyzed original materials and published the results of U-Pb, Ar-Ar, Rb-Sr, and Sm-Nd isotopic studies in Tuva, the Shoriya Mountains, Kuznetsk Alatau, and Batenev Range. | |
dc.subject | Paleozoic | |
dc.title | EARLY PALEOZOIC GRANITOID BATHOLITHS OF THE ALTAI-SAYAN FOLDED REGION (LATERAL-TEMPORAL ZONING AND SOURCES) | |
dc.type | Статья | |
dc.subject.age | Paleozoic | |
dc.subject.age | Палеозой | ru |
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