期刊
MINERALS
卷 10, 期 11, 页码 -出版社
MDPI
DOI: 10.3390/min10111000
关键词
Siberian craton; Verkhoyansk– Kolyma folded area; dike magmatism; U– Pb zircon dating; SHRIMP II SIMS; geodynamics; Yana– Kolyma gold belt
资金
- Diamond and Precious Metals Geology Institute, Siberian Branch of the Russian Academy of Sciences
- Russian Foundation for Basic Research [18-45-140040 r_a, 18-05-00854, 18-05-70035, 20-05-00360]
- Russian Science Foundation [19-17-00091]
We present the results of geostructural, mineralogic-petrographic, geochemical, and U-Pb geochronological investigations of mafic, intermediate, and felsic igneous rocks from dikes in the Yana-Kolyma gold belt of the Verkhoyansk-Kolyma folded area (northeastern Asia). The dikes of the Vyun deposit and the Shumniy occurrence intruding Mesozoic terrigenous rocks of the Kular-Nera and Polousniy-Debin terranes were examined in detail. The dikes had diverse mineralogical and petrographic compositions including trachybasalts, andesites, trachyandesites, dacites, and granodiorites. The rocks showed significant similarities in distributions of REE, and their concentrations of most HFSEs were close to the intermediate ones between ocean islands basalts and enriched middle ocean ridge basalts. We propose that the subduction that was ongoing during the collision of the Kolyma-Omolon superterrane with Siberia led to melting in the asthenospheric wedge and in the lithosphere, which formed a mixed source for the dike systems from both an enriched and a depleted mantle source. The U-Pb SHRIMP-II dates obtained for the dikes corresponded to the Late Jurassic interval of 151-145 Ma. We present a geodynamic model for the northeastern margin of the Siberian Craton for the Tithonian age of the Late Jurassic.
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