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首页> 外文期刊>Записки Российского минералогического общества >GUTKOVAITE-Mn, CaK_2Mn(Ti,Nb)_4(Si_4O_(12))_2(O,OH)_4 centre dot 5H_2O, A NEW MINERAL OF THE LABUNTSOVITE GROUP FROM KHIBINY MASSIF, KOLA PENINSULA
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GUTKOVAITE-Mn, CaK_2Mn(Ti,Nb)_4(Si_4O_(12))_2(O,OH)_4 centre dot 5H_2O, A NEW MINERAL OF THE LABUNTSOVITE GROUP FROM KHIBINY MASSIF, KOLA PENINSULA

机译:GUTKOVAITE-Mn,CaK_2Mn(Ti,Nb)_4(Si_4O_(12))_ 2(O,OH)_4中心点5H_2O,来自可拉宾州基比尼·马斯西夫的蓝宝石集团的新矿物

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摘要

Gutkovaite-Mn, a new mineral of the labuntsovite group, has been found at Maly Mannepakhk Mt., Khibiny alkaline massif, Kola peninsula, Russia. It occurs in pegmatite among nepheline syenite, with microcline, aegirine, arfvedsonite, nepheline, eudialyte, albite, lorenzenite, loparite, aenigmatite, mangan-neptunite, murmanite, analcime, natrolite, stilbite, chabazite, kuzmenkoite-Mn, nontronite, etc. it forms coarse-prismatic crystals up to 0.8mm in lenght. Translucent to transparent; pale yellowish-pink; streak white; luster vitreous. Brittle, cleavage not observed, fracture uneven. Mohs' hardness approx 5. D_(meas) 2.83, D_(calc) 2.70 g/cm~3. Optically biaxial, positive; alpha=1.688, beta=1.700, gamma=1.805; 2V_(meas)=35(10 deg). Chemical composition (microprobe data), wt percent: Na_2O 0.18, K_2O 6.54, CaO 4.81 SrO 0.54, BaO 1.03, MgO 0.17, MnO 4.96, FeO 0.61, ZnO 0.13, Al_2O_3 0.17, SiO_2 41.03, ZrO_2 0.08, TiO_2 24.47, Nb_2O_5 5.14, H_2O (calc.) 8.67. Total 98.53. Empirical formula calculated by [(Si,Al)_(16)O_(48)](O,OH)_8 is: (Ca_(2.00)Na_(0.14) sum_(2.14)(K_(3.24)Ba_(0.16)Sr_(0.12)sum_(3.52)(Mn_(1.63)~(2+)Fe_(0.20)Mg_(0.10)Zn_(0.04)sum_(1.97)(Ti_(7.14)Nb_(0.90)Zr_(0.02)sum_(8.06)[(Si_(15.92)Al_(0.08)sum_(16)O_(48))[O_(4.94)(OH)_(3.06)]sum_8 centre dot 9.7H_2O. Idealized formula is: CaK_2Mn(TiNb)_4(Si_4O_(12)_2(O,OH)_4 centre dot 5H_2O (Z=2). Crystal structure is studied; R=0.058. Monoclinic, space group Cm. Microtwinning by planes (001) and (-401) is observed. Unit cell parameters: a=14.30, b=13.889, c=7.760A, beta=117.51 deg, V=1367 A~3. Structurally related to labuntsovite but A-site occupied with Na in labuntsovite, has been subdivided into two sites in gutkovaite-Mn: A(I)-site is occupied with Ca selectively, A(II)-site is vacant. It's a cause of summetry lowering from C2/m (labuntsovite) to Cm (gutkovaite). Strongest reflexes of X-ray powder pattern are (d, A-I[hkl]): 7.0-7[020,001], 6.33-5[20-1,200], 4.90-4[021], 3.22-9[42-1, 40-2, 400], 3.05-10[022,24-1,240], 2.57-5[24-2,241], 2.48-6[44-1,40-3,401]. IR spectrum is given. Gutkovaite-Mn is named in the memory of Russian mineralogist N.N. Gutkova [1896-1960(?)] who intensively studied Khibiny-Lovozero alkaline complex, and Mn prevailing in D-site. Type specimen is deposited in Fersman Mineralogical Museum of Russian Academy of Sciences, Moscow.
机译:在俄罗斯科拉半岛Khibiny碱性地块的Maly Mannepakhk山发现了Labtsovite组的一种新矿物Gutkovaite-Mn。它发生在霞石正长岩中的伟晶岩中,与微晶岩,a庚因,阿夫韦德钠石,霞石,共沸石,钠长石,菱锰矿,钠钙铝石,钠长石,锰-海磷灰石,锰铁矿,方铁矿,钠铝石,钠长石,菱锰矿,钙长石,钙长石,钙长石,钙长石等形成长度达0.8mm的粗棱晶。半透明到透明;淡黄粉色条纹白色玻璃光泽。脆,未观察到分裂,断裂不均匀。莫氏硬度约为5。D_(平均)2.83,D_(计算)2.70 g / cm〜3。光学双轴正alpha = 1.688,beta = 1.700,gamma = 1.805; 2V_(测量)= 35(10度)。化学成分(探针数据),重量百分比:Na_2O 0.18,K_2O 6.54,CaO 4.81 SrO 0.54,BaO 1.03,MgO 0.17,MnO 4.96,FeO 0.61,ZnO 0.13,Al_2O_3 0.17,SiO_2 41.03,ZrO_2 0.08,TiO_2 24.47,Nb_2O_5 ,H_2O(计算值)8.67。总计98.53。由[[Si,Al] _(16)O_(48)] [O,OH)_8计算的经验公式为:(Ca_(2.00)Na_(0.14)sum_(2.14)(K_(3.24)Ba_(0.16)Sr_ (0.12)sum_(3.52)(Mn_(1.63)〜(2+)Fe_(0.20)Mg_(0.10)Zn_(0.04)sum_(1.97)(Ti_(7.14)Nb_(0.90)Zr_(0.02)sum_(8.06) [(Si_(15.92)Al_(0.08)sum_(16)O_(48))[O_(4.94)(OH)_(3.06)] sum_8中心点9.7H_2O。理想化公式为:CaK_2Mn(TiNb)_4(Si_4O_( 12)_2(O,OH)_4中心点5H_2O(Z = 2)。研究晶体结构; R = 0.058。单斜晶系,空间群Cm。观察到由平面(001)和(-401)产生的孪晶。 :a = 14.30,b = 13.889,c = 7.760A,β= 117.51deg,V = 1367A〜3。在结构上与Labuntsovite有关,但A位被Labuntsovite中的Na占据,已被细分成在Gutkovaite-Mn中的两个位点。 :A(I)位点被Ca选择性地占据,A(II)位点是空位的,这是总重量从C2 / m(凹凸棒石)降低到Cm(角铁矾)的原因,X射线粉末图案的反射最强是(d,AI [hkl]):7.0-7 [020,001],6.33-5 [20-1,200],4.90-4 [021],3.22-9 [42-1、40-2、400] ,3.05-10 [022,24-1,240],2.57-5 [24-2,241],2.48-6 [44-1,40-3,401]。给出了红外光谱。 Gutkovaite-Mn以纪念俄​​罗斯矿物学家N.N. Gutkova [1896-1960(?)]深入研究了Khibiny-Lovozero碱性络合物和Mn在D位点占主导地位。类型标本存放在莫斯科俄罗斯科学院的费斯曼矿物学博物馆。

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