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首页> 外文期刊>The American mineralogist >Footemineite, the Mn-analog of atencioite, from the Foote mine, Kings Mountain, Cleveland County, North Carolina, USA, and its relationship with other roscherite-group minerals
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Footemineite, the Mn-analog of atencioite, from the Foote mine, Kings Mountain, Cleveland County, North Carolina, USA, and its relationship with other roscherite-group minerals

机译:来自美国北卡罗来纳州克利夫兰县金斯山的Foote矿的脚铁矿的锰类似物Footemineite及其与其他红钙石类矿物的关系

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Footemineite, ideally Ca2Mn2+square Mn22+Be4(PO4)(6)(OH)(4)-6H(2)O, triclinic, is a new member of the roscherite group. It occurs on thin fractures crossing quartz-microcline-spodumene pegmatite at the Foote mine, Kings Mountain, Cleveland County, North Carolina, U.S.A. Associated minerals are albite, analcime, eosphorite, siderite/rhodochrosite, fairfieldite, fluorapatite, quartz, milarite, and pyrite. Footemineite forms prismatic to bladed generally rough to barrel-shaped crystals up to about 1.5 mm long and I mm in diameter. Its color is yellow, the streak is white, and the luster is vitreous to slightly pearly. Footemineite is transparent and non-fluorescent. Twinning is simple, by reflection, with twin boundaries across the length of the crystals. Cleavage is good on {0 (1) over bar1}) and {100}. Density (calc.) is 2.873 g/cm(3). Footemineite is biaxial (-), n(alpha) = 1.620(2), n(beta) = 1.627(2), n(gamma) = 1.634(2) (white light). 2V(obs) = 80 degrees, 2V(calc) = 89.6 degrees. Orientation: X boolean AND b similar to 12 degrees, Y boolean AND c similar to 15 degrees, Z boolean AND a similar to 15 degrees. Elongation direction is c, dispersion: r > v or r < v, weak. Pleochroism: beta (brownish yellow) > alpha = gamma (yellow). Mossbauer and IR spectra are given. The chemical composition is (EDS mode electron microprobe, Li and Be by ICP-OES, Fe3+:Fe2+ y Mossbauer, H2O by TG data, wt%): Li2O 0.23, BeO 9.54, CaO 9.43, SrO 0.23, BaO 0.24, MgO 0.18, MnO 26.16, FeO 2.77, Fe2O3 0.62, Al2O3 0.14, P2O5 36.58, SiO2 0.42, H2O 13.1, total 99.64. The empirical formula is (Ca1.89Sr0.03Ba0.02)Sigma(1.94)(Mn-0.90(2+)square(0.10))Sigma(1.00)(square 0.78Li0.17Mg0.05) Sigma(1.00)(Mn3.252+Fe0.432+ Fe0.093+Al0.03)Sigma(3.80) Be-4.30(P5.81Si0.08O24)[(OH)3.64(H2O)0.36]Sigma(4.00)center dot 6.00H(2)O . The strongest reflection peaks of the powder diffraction pattern [d, angstrom (1, %) (hkl)] are 9.575 (53) (010), 5.998 (100) (0 (1) over bar1), 4.848 (26) (021), 3.192 (44) (210), 3.003 (14) (0 (2) over bar2), 2.803 (38) ((1) over bar 03), 2.650 (29) ((2) over bar 02), 2.424 (14) (231). Single-crystal unit-cell parameters are a = 6.788(2), b = 9.972(3), c = 10.014(2) A, (x = 73.84(2), beta = 85.34(2), gamma = 87.44(2)degrees,V = 648.74 angstrom(3), Z = 1. The space group is P (1) over bar. Crystal structure was refined to R = 0.0347 with 1273 independent reflections (F > 2(5). Footemineite is dimorphous with roscherite, and isostructural with atencioite. It is identical with the mineral from Foote mine described as "triclinic roscherite." The name is for the Foote mine, type locality for this and several other minerals.
机译:最好是Ca2Mn2 +方Mn22 + Be4(PO4)(6)(OH)(4)-6H(2)O(三斜晶)的脚铁矿是roscherite组的新成员。它发生在美国北卡罗来纳州克利夫兰县金斯山的Foote矿上穿过石英-微晶石-锂辉石伟晶岩的细裂缝上。伴生的矿物有钠长石,方沸石,辉绿岩,菱铁矿/菱锰矿,费尔菲尔德岩,氟磷灰石,石英,珍珠岩和黄铁矿。 。钙钛矿形成棱柱形至刃状的,通常粗糙至桶状的晶体,长约1.5mm,直径约1mm。它的颜色是黄色,条纹是白色,光泽是玻璃态到略带珍珠色。钙钛矿是透明的和非荧光的。通过反射,孪晶很简单,在晶体的整个长度上都有孪晶边界。 {0(1)超过bar1})和{100}的切割效果良好。密度(计算)为2.873 g / cm(3)。针铁矿是双轴的(-),nα= 1.620(2),nβ= 1.627(2),nγ= 1.634(2)(白光)。 2V(obs)= 80度,2V(calc)= 89.6度。方向:X布尔值和b近似于12度,Y布尔值和c近似于15度,Z布尔值和a近似于15度。伸长方向是c,色散:r> v或r alpha =伽玛(黄色)。给出了莫斯鲍尔光谱和红外光谱。化学成分为(EDS模式电子探针,ICP-OES的Li和Be,Mossbauer的Fe3 +:Fe2 + y,TG数据的H2O,wt%):Li2O 0.23,BeO 9.54,CaO 9.43,SrO 0.23,BaO 0.24,MgO 0.18 ,MnO 26.16,FeO 2.77,Fe2O3 0.62,Al2O3 0.14,P2O5 36.58,SiO2 0.42,H1O 13.1,总计99.64。经验公式为(Ca1.89Sr0.03Ba0.02)Sigma(1.94)(Mn-0.90(2+)平方(0.10))Sigma(1.00)(平方0.78Li0.17Mg0.05)Sigma(1.00)(Mn3。 252 + Fe0.432 + Fe0.093 + Al0.03)Sigma(3.80)Be-4.30(P5.81Si0.08O24)[(OH)3.64(H2O)0.36] Sigma(4.00)中心点6.00H(2)O 。粉末衍射图的最强反射峰[d,埃(1,%)(hkl)]为9.575(53)(010),5.998(100)(0(1)over bar1),4.848(26)(021) ),3.192(44)(210),3.03(14)(bar 2上方的0(2)),2.803(38)(bar 03上方的(1)),2.650(29)(bar 02上方的(2)),2.424 (14)(231)。单晶晶胞参数为a = 6.788(2),b = 9.972(3),c = 10.014(2)A,(x = 73.84(2),beta = 85.34(2),gamma = 87.44(2 )度,V = 648.74埃(3),Z =1。空间群为P(1)(bar之上)。晶体结构细化到R = 0.0347,具有1273个独立反射(F> 2(5)。钙钛矿,以及与辉绿岩的同质结构,它与来自Foote矿的被称为“三斜辉红岩”的矿物相同。该名称取自Foote矿,此矿和其他几种矿物的类型局部。

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