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机译:透辉石-(OH),一种透辉石系列的新矿物,Mg2(BO3)1-x(SiO4)x(F,OH)1-x(x <0.5),来自俄罗斯萨哈-雅库特共和国的Snezhnoye矿床
Faculty of Earth Sciences, Department of Geochemistry, Mineralogy and Petrography, University of Silesia, Bdziska 60, 41-200 Sosnowiec, Poland;
CNR, Institute of Geosciences and Earth Resources (IGG), Unit of Pavia, Via A. Ferrata 1, I-27100 Pavia, Italy;
Mineralogical Crystallography, Institute of Geological Sciences, University of Bern, Freiestrasse 3, CH-3012 Bern, Switzerland;
Mineralogical Crystallography, Institute of Geological Sciences, University of Bern, Freiestrasse 3, CH-3012 Bern, Switzerland;
Faculty of Earth Sciences, Department of Geochemistry, Mineralogy and Petrography, University of Silesia, Bdziska 60, 41-200 Sosnowiec, Poland;
Institute of Geochemistry, Mineralogy and Petrology, University of Warsaw, al. wirki i Wigury 93, 02-089 Warszawa, Poland;
August Chekowski Institute of Physics, University of Silesia, Uniwersytecka 4, 40-007 Katowice, Poland;
机译:钙钛矿-(OH),是钠钙矿系列中的一种新矿物,Mg _2(BO_3)_(1-x)(SiO_4)_x(F,OH)_(1-x)(x <0.5),来自Snezhnoye矿床在俄罗斯萨哈-雅库特共和国
机译:Pertsevite是一种新的硅质镁硼酸盐矿物,其端部成分为Mg_2BO_3F,位于俄罗斯萨哈-雅库特州Verkhoyansk以东的科托特大理石中
机译:钾辉石(Nb,Mo)S_2-(Mg_(1-x)Al_x)(OH)_(2 + x),钾盐(Mo,Nb)S_2-(Mg_(1-x)Al_x)(OH)_(2 + x)+ x和manganokaskasite(Mo,Nb)S_2-(Mn_(1-x)Al_x)(OH)_(2 + x)来自俄罗斯科拉半岛Khibiny碱性复合物的三种新的堇青石族矿物
机译:衬底和氧退火对脉冲激光沉积La / sub 0.5 / Ca / sub 0.5 / Mn / sub 1-x / M / sub x / O / sub 3 /(M = Fe,Ni)薄膜的影响
机译:一系列低掺杂的结构和磁性 Zn $ _ {1-x} $ Co $ _x $ O从(0001)上的Zn和Co金属靶沉积的薄膜 al $ _2 $ O $ _3 $基板