Titlebook: Alkaline Rocks, Kimberlites and Carbonatites: Geochemistry and Genesis; Proceedings of the X Nikolay Vladykin Conference proceedings 2021 T

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轻快带来危险

Problems of Mantle Structure and Compositions of Various Terranes of Siberian Craton,80000). Geochemical features of the minerals have been determined by LA ICP MS. Mantle sections consist of 6–7 paleo-subducted slab separated by pyroxenite, eclogite and dunite lenses, disturbed by later plume melt intrusion accompanied by metasomatism and melting. The cross-sections and long transe

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Geochemistry, Mineralogy and Ore Content of Alkaline Granite Magmatism of East Sayan Zone (On the Eerentiation degree and ore potential, the rare-metal granites are divided into three facies varieties: early facies involving microcline-albite amphibole-bearing granites, middle facies represented by leucocratic quartz-albite granites, and late facies including essentially pure albite varieties. Pu

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琐碎

Crystal-Chemical Features of Rare and Complex Silicates from Charoite Rocks of the Malyy Murun Volcmplex silicates found out in the rocks of the Malyy Murun massif—the eastern part of the Murun volcano-plutonic alkaline complex. Murun complex is the world‘s largest massif of potassium-carbonated alkaline rocks; it is located on the southwestern edge of the Aldan Shield, on the border of Yakutia a

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GLIDE

Composition and Mechanisms of Formation of Comendite Melts of the Early Mesozoic Bimodal Associatiothe melts involved in the formation of comendites of the bimodal association of Sant’s volcanites (Central Mongolia), the mechanisms of their formation were revealed. Primary melt inclusions and crystalline inclusions coexisting with them were studied in quartz in three samples of comendites selecte

transplantation

Composition and Parameters of Generation of Primary Magma of Ultramafic Massif Uitkomst: Thermobaroh levels of MgO (up to 22.5 wt%), FeO, SiO. and LREE, the content of CaO, alkalis, volatiles and fluid-mobile components. Melting of magma took place at a temperature of 1590 °C and a pressure of 2.5 GPa. The main process of magma evolution in the early stages was crystallization differentiation, wh