Early Cretaceous Granitic and Monzonitic Rocks of the Southern Part of the Zhuravlevka Terrane (Sikhote-Alin): Geochemical Composition and Melt Sources
- Авторы: Kruk N.1,2, Gvozdev V.3, Orekhov A.3, Kruk E.1, Kasatkin S.3, Golozubov V.3, Rudnev S.1, Aoki S.4, Komiya T.5, Kovach V.6, Serov P.7
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Учреждения:
- Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences
- Novosibirsk State University
- Far East Geological Institute, Far East Branch, Russian Academy of Sciences
- Okayama University of Science
- Tokyo University
- Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences
- Geological Institute, Kola Science Center, Russian Academy of Sciences
- Выпуск: Том 13, № 3 (2019)
- Страницы: 220-238
- Раздел: Article
- URL: https://journals.rcsi.science/1819-7140/article/view/211628
- DOI: https://doi.org/10.1134/S1819714019030047
- ID: 211628
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Аннотация
The article presents new geological, geochronological, mineralogical, geochemical, and isotopic data on the Early Cretaceous granitic rocks of the southern part of the Zhuravlevka Terrane (Sikhote-Alin). It is shown that four intrusive complexes containing significant amounts of granitic rocks were formed almost simultaneously in this area in the Early Cretaceous (about 100 Ma). These magmatic associations differ in rock set, their mineralogical characteristics, and chemical composition, varying from medium-potassium tonalites and granodiorites depleted in incompatible elements to shoshonitic monzonitic rocks enriched in HFSE and REE. The geochemical and isotopic characteristics of the granitic rocks indicate that the source of their melts was dominated by essentially juvenile metabasite crust with a limited contribution of the upper-crustal metasedimentary rocks. The diversity of geochemical types of the granitic rocks is explained by variable metabasite and metapelite contributions to their source, upper crustal contamination during magma ascent, as well as the variable contribution of the mantle source and different mechanisms of mantle–crust interaction.
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Об авторах
N. Kruk
Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences; Novosibirsk State University
Автор, ответственный за переписку.
Email: kruk@igm.nsc.ru
Россия, pr. Akademika Koptyuga 3, Novosibirsk, 630090; ul. Pirogova 2, Novosiborsk, 630090
V. Gvozdev
Far East Geological Institute, Far East Branch, Russian Academy of Sciences
Email: serov@geoksc.apatity.ru
Россия, pr. 100-letiya Vladivostoku 159, Vladivostok, 690022
A. Orekhov
Far East Geological Institute, Far East Branch, Russian Academy of Sciences
Email: serov@geoksc.apatity.ru
Россия, pr. 100-letiya Vladivostoku 159, Vladivostok, 690022
E. Kruk
Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences
Автор, ответственный за переписку.
Email: nn@mail.ru
Россия, pr. Akademika Koptyuga 3, Novosibirsk, 630090
S. Kasatkin
Far East Geological Institute, Far East Branch, Russian Academy of Sciences
Email: serov@geoksc.apatity.ru
Россия, pr. 100-letiya Vladivostoku 159, Vladivostok, 690022
V. Golozubov
Far East Geological Institute, Far East Branch, Russian Academy of Sciences
Автор, ответственный за переписку.
Email: golozubov@fegi.ru
Россия, pr. 100-letiya Vladivostoku 159, Vladivostok, 690022
S. Rudnev
Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences
Email: serov@geoksc.apatity.ru
Россия, pr. Akademika Koptyuga 3, Novosibirsk, 630090
Sh. Aoki
Okayama University of Science
Email: serov@geoksc.apatity.ru
Япония, Okayama
T. Komiya
Tokyo University
Email: serov@geoksc.apatity.ru
Япония, Tokyo
V. Kovach
Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences
Автор, ответственный за переписку.
Email: v.kovach@mail.ru
Россия, nab. Makarova 2, St. Petersburg, 1190034
P. Serov
Geological Institute, Kola Science Center, Russian Academy of Sciences
Автор, ответственный за переписку.
Email: serov@geoksc.apatity.ru
Россия, ul. Fersmana 14, Apatity, 184209