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.
机构:
Russian Acad Sci, Inst Geol Ore Deposits Petrog Mineral & Geochem, Moscow 119017, RussiaRussian Acad Sci, Inst Geol Ore Deposits Petrog Mineral & Geochem, Moscow 119017, Russia
Yarmolyuk, V. V.
Lykhin, D. A.
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机构:
Russian Acad Sci, Inst Geol Ore Deposits Petrog Mineral & Geochem, Moscow 119017, RussiaRussian Acad Sci, Inst Geol Ore Deposits Petrog Mineral & Geochem, Moscow 119017, Russia
Lykhin, D. A.
Shuriga, T. N.
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机构:
All Russia Res Inst Mineral Resources, Moscow 119017, RussiaRussian Acad Sci, Inst Geol Ore Deposits Petrog Mineral & Geochem, Moscow 119017, Russia