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High-Phosphorous Lithium-Fluorine Granites of Eastern Yakutia (Verkhoyansk-Kolyma Orogenic Region)

机译:雅库特东部的高磷锂 - 氟花岗岩(Verkhoyansk-Kolyma Oreganic地区)

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摘要

The paper considers the petrographic composition and petro- and geochemical features of high-phosphorous lithium-fluorine granites from the Arga-Ynnakh-Khaya and Burgali ore-magmatic clusters in eastern Yakutia. Granitoids of three successively formed petrotypes are recognized here: amphibole-biotite granodiorites and andesine granites close to I-type granitoids; S-type two-mica cordierite granites; and plumasite lithium-fluorine granites. The latter are characterized by extremely high Li, Cs, F, and P contents; they are ascribed to ultra-rare-metal rocks and are not complementary to the preceding granitoids. They are assumed to be the derivatives of independent melts obtained from a lower crustal protolith that was reworked by ore- and volatile-rich fluids related to upwelling subalkaline or alkaline basaltic melts.
机译:本文考虑了来自雅库特岛氨基·克什 - 哈伊亚和Burgali矿石群的高磷锂 - 氟花岗岩的岩体成分和地球化学特征。 此处认识到三个连续形成的近型的花岗岩:Amphibole-Biotite Granodiorites和靠近I型花岗岩的andesine花岗岩; S型双云母堇青石花岗岩; 和褶皱锂 - 氟花岗岩。 后者的特征在于极高的Li,CS,F和P含量; 它们归因于超稀有金属岩石,并不与前面的花岗岩互补。 假设它们是由较低的地壳促果实获得的独立熔体的衍生物,其通过与升高的亚甲醇或碱性玄武岩熔体有关的矿石和富含氟的液体再加工。

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