Пожалуйста, используйте этот идентификатор, чтобы цитировать или ссылаться на этот ресурс:
http://hdl.handle.net/11701/44840
Полная запись метаданных
Поле DC | Значение | Язык |
---|---|---|
dc.contributor.author | Kuznetsov, Maksim V. | - |
dc.contributor.author | Savatenkov, Valery M. | - |
dc.date.accessioned | 2024-02-06T14:37:11Z | - |
dc.date.available | 2024-02-06T14:37:11Z | - |
dc.date.issued | 2023-09 | - |
dc.identifier.citation | Kuznetsov, M. V., Savatenkov, V. M. (2023). Melting modeling of mixed peridotitic and mafic lithologies at shallow depths of the continental metasomatized lithospheric mantle: Implementation for the Early Cretaceous volcanic rocks of Eastern Mongolia. Vestnik of Saint Petersburg University. Earth Sciences, 68 (3), 596–617. https://doi.org/10.21638/spbu07.2023.309 | en_GB |
dc.identifier.other | https://doi.org/10.21638/spbu07.2023.309 | - |
dc.identifier.uri | http://hdl.handle.net/11701/44840 | - |
dc.description.abstract | The Eastern Mongolia volcanic area formed in the Late Mesozoic — Early Cenozoic within Central Asian Orogenic Belt. The main volcanic events of the area occurred in the Early Cretaceous when alkaline basaltic lavas erupted and formed the so-called cover volcanic complex. Geochemical and isotope features of the cover volcanic complex allowed researchers to identify the following mantle rocks as their source: metasomatized peridotites, eclogites, and pyroxenites. Thermodynamic modeling in alphaMELTS program was performed to determine whether the simultaneous melting of these rocks with subsequent processes of crystallization differentiation could lead to the formation of the studied rocks. The modeling results show that the melting of the most enriched with incompatible trace elements peridotites, eclogites, and pyroxenites cannot produce the rocks of the cover volcanic complex. At the same time, the mixing of peridotite- and eclogite- derived melts corresponds most closely to the mechanism of rock formation. However, Ti, K, P, Rb, and Sr enrichment of the studied rocks also requires participation in magma generation processes of mantle metasomatic veins enriched with rutile, apatite, phlogopite, and amphibole. | en_GB |
dc.description.sponsorship | This work was subsidized by the Russian Science Foundation (project no. 23-27-00165) and the State Assignments of Institute of Precambrian Geology and Geochronology of the Russian Academy of Sciences no. FMUW-2022-0005. | en_GB |
dc.language.iso | en | en_GB |
dc.publisher | St Petersburg State University | en_GB |
dc.relation.ispartofseries | Vestnik of St Petersburg University. Earth Sciences;Volume 68; Issue 3 | - |
dc.subject | Eastern Mongolia | en_GB |
dc.subject | Early Cretaceous volcanism | en_GB |
dc.subject | thermodynamic modeling | en_GB |
dc.subject | eclogites | en_GB |
dc.subject | pyroxenites | en_GB |
dc.subject | mantle metasomatic veins | en_GB |
dc.title | Melting modeling of mixed peridotitic and mafic lithologies at shallow depths of the continental metasomatized lithospheric mantle: Implementation for the Early Cretaceous volcanic rocks of Eastern Mongolia | en_GB |
dc.type | Article | en_GB |
Располагается в коллекциях: | Issue 3 |
Файлы этого ресурса:
Файл | Описание | Размер | Формат | |
---|---|---|---|---|
09.pdf | 6,63 MB | Adobe PDF | Просмотреть/Открыть |
Все ресурсы в архиве электронных ресурсов защищены авторским правом, все права сохранены.