Volcanic rocks of the Khabarovsk accretionary complex, southern Far East Russia
- 作者: Voinova I.1
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隶属关系:
- Kosygin Institute of Tectonics and Geophysics, Far East Branch
- 期: 卷 10, 编号 3 (2016)
- 页面: 230-238
- 栏目: Article
- URL: https://journals.rcsi.science/1819-7140/article/view/211092
- DOI: https://doi.org/10.1134/S1819714016030076
- ID: 211092
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详细
The results of study of the volcanic rocks of the Khabarovsk accretionary complex, a fragment of the Jurassic accretionary prism of the Sikhote Alin orogenic belt (the southern part of the Russian Far East), are presented. The volcanic rocks are associated with the Lower Permian limestones in the mélange blocks and Triassic layered cherts. The petrography, petrochemistry, and geochemistry of the rocks are characterized and their geodynamic formation conditions are deduced. The volcanic rocks include oceanic plume basalts of two types: (i) OIB-like intraplate basalts formed on the oceanic islands and guyots in the Permian and Triassic and (ii) T(transitional)-MORBs (the least enriched basalts of the E-MORB type) formed on the midoceanic ridge in the Permian. In addition to basalts, the mélange hosts suprasubduction dacitic tuff lavas.
作者简介
I. Voinova
Kosygin Institute of Tectonics and Geophysics, Far East Branch
编辑信件的主要联系方式.
Email: ipvoinova@yandex.ru
俄罗斯联邦, ul. Kim Yu Chena 65, Khabarovsk, 680000