LA-ICP MS Characteristic of Geochemical Composition of Veins Rocks from the Central Part of the Khibina Massive in Kola Peninsula, Northern Russia

作     者：Milosz Huber 

作者机构：Optical and Electron Microscopy Laboratory Geology and Litosphere Protection Departament Earth Science and SpatialManagement Faculty Maria Curie-Sktodowska University Lublin 20-718 Poland 

出 版 物：《Journal of Chemistry and Chemical Engineering》 (化学与化工（英文版）)

年 卷 期：2014年第8卷第4期

页      面：364-370页

学科分类：081803[工学-地质工程] 08[工学] 0818[工学-地质资源与地质工程] 080502[工学-材料学] 0805[工学-材料科学与工程（可授工学、理学学位）] 

主　　题：Khibina Massive Kola Peninsula vein rocks geochemistry. 

摘      要：This paper discusses the vein rocks located in the central part of Khibina Mts.. These rocks are located on the border of two zones： ore and external. In the ore, zone is present titanite-nepheline bodies whilst in the outer zone are massive-syenites ＂khibinites＂. The veins can be divided into： mikrosyenites, melteigites and other rock types （e.g., tinguaites）. The results of LA-ICP MS （laser ablation of inductively coupled plasma mass spectrometry） indicate that these rocks are associated with deep zones which formed as a result of injection of primary magma and contamination of fluids during migration, where there have hydrothermal processes. Rock-forming minerals, their corrosion and accessory minerals indicate these processes, too.