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Katophorite from the Jade Mine Tract, Myanmar: mineral description of a rare (grandfathered) endmember of the amphibole supergroup

机译:缅甸翡翠矿区的钾镁辉石:闪石超群的罕见(祖父)末端成员的矿物描述

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Katophorite has the ideal formula Na-A(B)(NaCa)(C)(Mg4Al)(T)(Si7Al)O-22(W)(OH)(2) (Hawthorne et al., 2012). No published analyses of amphiboles fall in the katophorite compositional field, except that of Harlow and Olds (1987) for an amphibole from near Hpakan in the Jade Mine Tract, Myanmar. This amphibole was approved by the International Mineralogical Association Commission on New Minerals, Nomenclature and Classification (vote 2013-140) as katophorite, and is reported here. Holotype katophorite is monoclinic, space group C2/m, a = 9.8573(8), b = 17.9617(15), c = 5.2833(4) angstrom, b = 104.707(2)degrees, V = 904.78(13) angstrom(3), Z = 2. The calculated density is 3.091 g cm(-3). In plane-polarized light, katophorite is pleochroic, X = pale blue (medium), Y = light blue-green (strongest), Z = colourless; X boolean AND a = 30.6 degrees (beta obtuse), Y parallel to b, Z boolean AND c = 15.8 (beta acute). It is biaxial negative, alpha = 1.638, beta = 1.642, gamma = 1.644, all +/- 0.002; 2V(obs) = 73(1)degrees, 2V(calc) = 70 degrees. The eight strongest lines in the powder X-ray diffraction pattern are [d in angstrom (I)(hkl)]: 2.700 (100)(151), 3.129 (69)(310), 2.536 (65)((2) over bar 02), 3.378 (61)(131), 8.421 (55)(110), 2.583 (46)(061), 2.942 (43)(221) and 2.334 (41)((3) over bar 51). Electron-microprobe analysis of the refined crystal gave SiO2 51.74, Al2O3 7.38, TiO2 0.14, FeO 1.55, Fe2O3 2.82, MgO 18.09, CaO 8.17, Na2O 6.02, K2O 0.24, F 0.06, H2Ocalc. 1.80, Li2Ocalc. 0.09, sum 100.55 wt.% (Li2O and H2O based on the results of single-crystal structure refinement). The formula unit, calculated on the basis of 24 (O,OH,F) with (OH + F + O) = 2 is: (A)(Na0.85K0.04)(Sigma=0.89)(B)(Ca1.22Na0.78)(Sigma=2.00)(C)(Mg3.76Al0.43Fe0.303+Cr0.273+Fe0.182+Li0.05Ti0.014+)(Sigma=5.00)(T)(Si7.21Al0.79)(Sigma=8.00)O-22(W)[(OH)(1.67)O0.30F0.03)](Sigma=2.00).
机译:钾霞石具有理想的分子式Na-A(B)(NaCa)(C)(Mg4Al)(T)(Si7Al)O-22(W)(OH)(2)(Hawthorne et al。,2012)。除Harlow和Olds(1987)在缅甸翡翠矿区Hpakan附近的闪石外,没有任何已发表的闪石的分析属于该钾镁辉石的组成领域。该闪石被国际矿物学协会新矿物,命名学和分类委员会批准(票号2013-140)为钾镁辉石,并在此报道。整体型钾镁辉石为单斜晶系,空间群为C2 / m,a = 9.8573(8),b = 17.9617(15),c = 5.2833(4)埃,b = 104.707(2)度,V = 904.78(13)埃(3 ),Z =2。计算出的密度为3.091 g cm(-3)。在平面偏振光中,钾镁铝石是多色的,X =浅蓝色(中等),Y =浅蓝绿色(最强),Z =无色; X布尔值和a = 30.6度(β钝角),Y平行于b,Z布尔值和c = 15.8(β尖角)。它是双轴负值,alpha = 1.638,beta = 1.642,gamma = 1.644,全部+/- 0.002; 2V(obs)= 73(1)度,2V(calc)= 70度。粉末X射线衍射图中最强的八条线[d以埃(hk)为单位]:2.700(100)(151),3.129(69)(310),2.536(65)((2)over条51)上的第3.378(61)(131),8.421(55)(110),2.583(46)(061),2.942(43)(221)和2.334(41)((3))。精制晶体的电子探针分析得到SiO2 51.74,Al2O3 7.38,TiO2 0.14,FeO 1.55,Fe2O3 2.82,MgO 18.09,CaO 8.17,Na2O 6.02,K2O 0.24,F 0.06,H2Ocalc。 1.80,Li 2 Ocalc。 0.09,总计100.55 wt。%(基于单晶结构细化的结果,Li2O和H2O)。以(OH + F + O)= 2的24(O,OH,F)为基础计算的公式单位是:(A)(Na0.85K0.04)(Sigma = 0.89)(B)(Ca1。 22Na0.78)(Sigma = 2.00)(C)(Mg3.76Al0.43Fe0.303 + Cr0.273 + Fe0.182 + Li0.05Ti0.014 +)(Sigma = 5.00)(T)(Si7.21Al0.79 )(Sigma = 8.00)O-22(W)[(OH)(1.67)O0.30F0.03)](Sigma = 2.00)。

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