Geochemistry and Age of Basic Dikes of the Snezhnoe Be Deposit: Evidence for the Late Paleozoic Plume-Mantle Magmatism of East Sayan

被引:0
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作者
Khubanov, V. B. [1 ]
Dolgoborodova, K. D. [1 ]
Tsygankov, A. A. [1 ]
Khubanova, A. M. [1 ]
Damdinova, L. B. [1 ]
Damdinov, B. B. [1 ]
Burmakina, G. N. [1 ]
Zarubina, O. V. [2 ]
机构
[1] Russian Acad Sci, Dobretsov Geol Inst, Siberian Branch, Ulan Ude 670047, Russia
[2] Russian Acad Sci, Vinogradov Inst Geochem, Siberian Branch, Irkutsk 664033, Russia
基金
俄罗斯基础研究基金会;
关键词
Late Paleozoic; plume magmatism; asthenospheric mantle; East Sayan rare metal zone; Barguzin SLIP;
D O I
10.1134/S1028334X22601055
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Mafic subvolcanic bodies (gabbroids, mafic dikes) occur within the East Sayan rift zone of the Late Paleozoic Barguzin silicic large igneous province (SLIP) together with ore-bearing alkali granitoids. The Snezhnoe Be deposit is a typical object with a mafic-alkali granitoid association. The mafic dikes intruding the ore structures of the deposit are dated using the LA-ICP-MS U-Pb method. The age of zircons from the diabase (dolerite) and microgabbro dikes is 301 +/- 6 and 297 +/- 2 Ma, respectively. These ages are similar to that of fluorite-phenakite-beryllium mineralization (306 Ma) and associated alkali granites with Ta-Nb mineralization, which are ascribed to the Ognit complex (311-295 Ma). The geochemical features of mafic dikes suggests the generation of mafic magmas from an asthenospheric mantle source, which, taking into account the intracontinental setting, indicates in favor of a plume-mantle nature of mafic-alkali granitoid magmatism of the East Sayan rift (rare metal) zone, in particular, the entire Barguzin SLIP in general.
引用
收藏
页码:S251 / S256
页数:6
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