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首页> 外文期刊>American Mineralogist >Pertsevite-(OH), a new mineral in the pertsevite series, Mg2(BO3)1-x(SiO4)x(F,OH)1-x (x < 0.5), from the Snezhnoye deposit in Sakha-Yakutia Republic, Russia
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Pertsevite-(OH), a new mineral in the pertsevite series, Mg2(BO3)1-x(SiO4)x(F,OH)1-x (x < 0.5), from the Snezhnoye deposit in Sakha-Yakutia Republic, Russia

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

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摘要

Pertsevite-(OH), end-member formula Mg2(BO3)(OH), is a new mineral found in a ludwigite-kotoite magnesian skarn from the Snezhnoye deposit in Sakha-Yakutia Republic, Russia. The Commission on New Minerals, Nomenclature and Classification, IMA (IMA 2008-060) has approved the mineral and the mineral name. Moreover, the Chairman of the CNMNC agreed to renaming pertsevite to pertsevite-(F). The two minerals constitute the pertsevite series with the general formula Mg2(BO3)1–x (SiO4)x(OH,F)1–x, where x = 0.1–0.3. Pertsevite-(OH) is biaxial: 2Vz = 55–65°(meas), 2Vz = 75°(calc); = 1.611(1), β = 1.623(1), gamma; = 1.644(1)°; X = b, Y = c, Z = a. It is associated with kotoite, szaibelyite, ludwigite-azoproite, clinohumite, hydroxylclinohumite, forsterite, chondrodite, calcite, REE-bearing sakhaite, sphalerite, and goethite. Ion microprobe analyses of pertsevite-(OH) using secondary ion mass spectrometry gave B, F, and H contents consistent with B and F contents determined by electron microprobe analyses (EMPA), and with OH contents calculated from EMPA data, confirming that OH/F ratio > 1 in pertsevite-(OH). Pertsevite-(OH) is orthorhombic, with space group Pnma. Cell dimensions refined from X-ray powder diffraction data are as follows: a = 20.499(1), b = 11.900(1), c = 4.589(1) Å, and V = 1119.4(3) Å3. The strongest lines of the X-ray diffraction pattern are [(hkl), d-spacing in Å, (I)]: (331) 2.7480 (61), (141) 2.4788 (42), (711) 2.4197 (35), (441) 2.2455 (86), (801) 2.2408 (45), (442) 1.7124 (100), (802) 1.7074 (47), and (12.4.0) 1.4817 (51). The main bands in the FTIR spectrum of pertsevite-(OH) are 1354, 1261, 1178, 1022, 975, 929, 888, 745, 555 and OH-specific 3696, 3562, 3530 cm–1.
机译:钙钛矿-(OH),端基分子式为Mg 2 (BO 3 )(OH),是一种新的矿物 ,在路德维希岩中发现-来自俄罗斯萨哈-雅库特共和国Snezhnoye 矿床的kotoite镁质矽卡岩。 IMA 新矿物,术语和分类委员会(IMA 2008-060) 批准了矿物和矿物名称。此外,CNMNC主席 同意将白云母重命名为Pertsevite-(F)。 这两种矿物质组成了具有通用 公式的白云母系列。 Mg 2 (BO 3 1-x (SiO 4 x ( OH,F) 1-x ,其中x = 0.1-0.3。钙钛矿-(OH)是双轴的:2V z = 55–65°(meas), 2V z = 75°(calc); = 1.611(1),β= 1.623(1),伽马; = 1.644(1)°; X = b,Y = c,Z = a。它与 kotoite,szaibelyite,ludwigite-azoproite,clinohumite,hydroxyclinohumite, 镁橄榄石,长绒石,方解石,含稀土的方铁矿,闪锌矿, 和针铁矿。使用 二次离子质谱法对钙钛矿-(OH)进行离子微探针分析,得出的B,F和H含量与通过电子探针分析测定的B和F含量一致 (EMPA),并根据EMPA数据计算出OH含量,从而确认 钙镁矿-(OH)中的OH / F比> 1。钙钛矿-(OH)是 斜方晶系,空间群为Pnma。从X射线粉末衍射数据细化的 像元尺寸如下:a = 20.499(1), b = 11.900(1),c = 4.589(1)Å,并且V = 1119.4(3)Å 3 X射线衍射图的最强线是[(hkl), d间距inÅ,(I)]:(331)2.7480(61),(141)2.4788 (42),(711)2.4197(35),(441)2.2455(86),(801) 2.2408(45), (442)1.7124(100),(802)1.7074(47)和(12.4.0)1.4817(51)。 钙钛矿-(OH)的FTIR光谱为1354, 1261,1178,1022,975,929,888,745,555和OH-specific 3696, 3562,3530 cm –1

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  • 来源
    《American Mineralogist》 |2010年第7期|953-958|共6页
  • 作者单位

    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;

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