First results of zircon LA-ICP-MS U-Pb dating of the rocks from the Granulite complex of Khanka massif in the Primorye region

This work is dedicated to the first results of zircon LA-ICP-MS U-Pb dating of the rocks from the granulite complex of the Khanka Massif in the Primorye region. Similar to the Khingan-Bureya (Russia) and Jiamusi (China) terranes, the Khanka Massif (terrane) represents one of the principal structural...

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Published inDoklady earth sciences Vol. 434; no. 1; pp. 1164 - 1167
Main Authors Khanchuk, A. I., Vovna, G. M., Kiselev, V. I., Mishkin, M. A., Lavrik, S. N.
Format Journal Article
LanguageEnglish
Published Dordrecht SP MAIK Nauka/Interperiodica 01.09.2010
Springer
Springer Nature B.V
Subjects
Crystallography
Dating
Earth and Environmental Science
Earth Sciences
Geochemistry
Geology
Isotopes
Massifs
Metamorphic rocks
Mineralogy
Rocks
Rocks, Metamorphic
Zircon
Zirconium
Primorye Russia
Back Scatter Electron Image
DOKLADY Earth Science
East Geological Institute
206Pb
Zircon
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Summary:This work is dedicated to the first results of zircon LA-ICP-MS U-Pb dating of the rocks from the granulite complex of the Khanka Massif in the Primorye region. Similar to the Khingan-Bureya (Russia) and Jiamusi (China) terranes, the Khanka Massif (terrane) represents one of the principal structural elements in the Near Pacific segment of the Central Asian fold belt. The age and origin of metamorphic rocks from these massifs are of importance for understanding the structural evolution of the latter. Granulite complexes of crystalline massifs in the Russian Far East are attributed to the Archean, although available isotopic dates are inconsistent with this standpoint. In this connection, isotopic geochronological studies of granulite rocks from the Khanka Massif are of particular significance.
Bibliography:ObjectType-Article-2
SourceType-Scholarly Journals-1
ObjectType-Feature-1
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ISSN:1028-334X
1531-8354
DOI:10.1134/S1028334X10090059