首页> 外文期刊>Geology of Ore Deposits: A Journal of Theoretical and Applied Papers on All Aspects of Ore Genesis >Fluorine-Beryllium Deposits of the Vitim Highland,Western Transbaikal Region:Mineral Types,Localization Conditions,Magmatism,and Age
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Fluorine-Beryllium Deposits of the Vitim Highland,Western Transbaikal Region:Mineral Types,Localization Conditions,Magmatism,and Age

机译:西泛贝加尔地区维蒂姆高地的氟铍矿床:矿物类型,定位条件,岩浆作用和年龄

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摘要

The fluorine-beryllium deposits of the Vitim Highland are represented by two mineral types:feldspar-fluorite-phenakite-bertrandite and thorite-fluorite-phenakite.Their localization is controlled by fault zones of various orders,folds,and stocks and dikes of the Early Mesozoic subalkali quartz syenite and syenite porphyry.The ore is represented by mineralized crush zones and metasomatic veins hosted in intercalated carbonate and aluminosilicate rocks.The deposits were formed under hydrothermal conditions at 360-90 deg C;their age is estimated at (243+-3)-(260+-2) Ma.
机译:维提姆高地的氟铍矿床由两种矿物类型代表:长石萤石-辉石-辉石-辉石-菱镁矿-萤石-辉石-辉石。它们的定位受早期不同阶次,褶皱,储量和堤防的断裂带控制。中生代次碱性石英正长岩和正长斑状斑岩,矿石以矿化的破碎带和交代脉为代表,埋藏在碳酸盐和铝硅酸盐岩层中,矿床是在360-90℃的热液条件下形成的,其年龄估计为(243 +- 3)-(260 + -2)马。

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