首页> 外文期刊>Записки Российского минералогического общества >TSEPINITE-Na (Na, H_3O, K, Sr, Ba)_2(Ti, Nb)_2(Si_4O_(12))(OH,O)_2 CENTRE DOT 3H_2O, A NEW MINERAL OF THE LABUNTSOVITE GROUP
【24h】

TSEPINITE-Na (Na, H_3O, K, Sr, Ba)_2(Ti, Nb)_2(Si_4O_(12))(OH,O)_2 CENTRE DOT 3H_2O, A NEW MINERAL OF THE LABUNTSOVITE GROUP

机译:TSEPINITE-Na(Na,H_3O,K,Sr,Ba)_2(Ti,Nb)_2(Si_4O_(12))(OH,O)_2 CENTER DOT 3H_2O,LABUNTSOVITE集团的新成员

获取原文
获取原文并翻译 | 示例
获取外文期刊封面目录资料

摘要

Tsepinite-Na, a new mineral of the labuntsovite group, has been found in alkaline pegmatites at Khibinpakhchorr Mt., Khibiny massif, and Lepkhe-Nelm Mt., Lovozero massif (both at Kola Peninsula. Russia). It occurs as colourless, white and light-brown radial aggregates and separate prismatic crystals (up to 1 cm) together with microcline, aegirine, analcime, natrolite, catapleiite, apophyllite, labuntsovite-Mn, epididymite, fluorite, sphalerite, etc. (Khibinpakhchorr) and with microcline, aegirine, magnesio-arfvedsonite, natrolite, eudialyte, lamprophyllite, fluorapatite, neptunite, lorenzenite, titanite, vinogradovite, polylithionite, tainiolite, rancieite, tundrite-(Ce) (Lepkhe-Nelm). Crystal forms: {001}, {100}, {2-bar 01}, {010}, {012}, {2-bar 41}. Transparent to translucent. Lustre vitreous. Brittle, cleavage is not observed, Mohs' hardness 5. D_(meas) = 2.74(2), D_(calc) = 2.72(1) g/cm~3. Optically biaxial, positive, #alpha# 1.658(1), #beta# 1.668(1), #gamma# 1.770(5), 2V_(meas) = 19-3l deg, 2V_(calc) = 36 deg. The crystal structure is studied, R = 0.055. Monoclinic, Cm, a = 14.604(7), b = 14.274(8), c = 7.933(2) A, #beta# = 117.40(3), V=1468.2 A~3. Tsepinite-Na is a structural analogue of vuoriyarvite-K with Na > K and Ti > Nb. Na~+ in tsepinite-Na is partly substituted with H_3O~+. Presence of H_3O~+ is confirmed by IR spectral data. The average chemical composition for the structurally studied crystal is (electron probe, wt percent): Na_2O 5.48, K_2O 1.58, CaO 0.18, SrO 2.32, BaO 2.60, ZnO 0.04, Fe_2O_3 0.25, TiO_2 14.17, Nb_2O_5 20.69, SiO_2 40.38, total 87.69. H_2O content (by thermogravimetrical procedure in vacuum) is 13.18 percent. The empirical formula is (Z = 1): H_(34.83)(Na_(4.21)K_(0.80)Sr_(0.54)Ba_(0.41)Zn_(0.01))#SIGMA#6.05(Ti_(4.22)Nb_(3.71)Fe_(0.07)~(3+))#SIGMA#8.00 Si_(16)O_(70.78). Idealized formula is (Z=4): (Na, H_3O, K, Sr, Ba)_2(Ti, Nb)_2(Si_4O_(12))(OH,O)_2 centre dot 3H_2O. The strongest reflexes of the X-ray powder pattern are (d, A (I, percent; hkl)): 7.01(44; 001), 6.46(100; 200, 2-bar 01), 3.954(30; 201, 2-bar 02), 3.236(98; 400, 4-bar 02), 3.179(33;041), 3.160(38;022). The mineral is named after Anatoliy I. Tsepin (b. 1946) who firstly obtained electron microprobe data for labuntsovite group minerals. Type specimen is Fersman Mineralogical Museum of the Russian Academy of Sciences, Moscow.
机译:Tsepinite-Na是Labuntsovite组的一种新矿物,已在Khibiny地块的Khibinpakhchorr山和Lovozero地块的Lepkhe-Nelm山的碱性伟晶岩中(均在俄罗斯可拉半岛)被发现。它以无色,白色和浅棕色放射状聚集体形式存在,并与独立的棱柱状晶体(长达1厘米)一起,与微线,aegirine,analcime,钠铁石,卡普莱石,appolitelite,labuntsovite-Mn,附睾,萤石,闪锌矿等一起出现(Khibinpakhchorr ),并使用微折线仪,aegirine,镁碱镁橄榄石,钠铝石,eudialyte,萤光沸石,氟磷灰石,n石、,石,钛铁矿,钛白云母,聚锂石,钛铁矿,褐铁矿,红闪石,芒硝-(Ce)(Lepkhe-Nelm)。晶形:{001},{100},{2-bar 01},{010},{012},{2-bar 41}。透明至半透明。玻璃光泽。观察不到脆性,开裂,莫氏硬度为5。D_(平均)= 2.74(2),D_(计算)= 2.72(1)g / cm〜3。光学双轴正正#alpha#1.658(1),#beta#1.668(1),#gamma#1.770(5),2V_(meas)= 19-3l度,2V_(calc)= 36度。研究了晶体结构,R = 0.055。单斜晶系,Cm,a = 14.604(7),b = 14.274(8),c = 7.933(2)A,#beta#= 117.40(3),V = 1468.2 A〜3。 Tsepinite-Na是vuoriyarvite-K的结构类似物,Na> K,Ti> Nb。菱沸石-Na中的Na〜+被H_3O〜+部分取代。红外光谱数据证实了H_3O〜+的存在。经结构研究的晶体的平均化学成分为(电子探针,重量百分比):Na_2O 5.48,K_2O 1.58,CaO 0.18,SrO 2.32,BaO 2.60,ZnO 0.04,Fe_2O_3 0.25,TiO_2 14.17,Nb_2O_5 20.69,SiO_2 40.38,总计87.69 。 H_2O含量(通过真空热重分析法测定)为13.18%。经验公式为(Z = 1):H_(34.83)(Na_(4.21)K_(0.80)Sr_(0.54)Ba_(0.41)Zn_(0.01))#SIGMA#6.05(Ti_(4.22)Nb_(3.71)Fe_ (0.07)〜(3 +))#SIGMA#8.00 Si_(16)O_(70.78)。理想的公式是(Z = 4):(Na,H_3O,K,Sr,Ba)_2(Ti,Nb)_2(Si_4O_(12))(OH,O)_2中心点3H_2O。 X射线粉末图案的最强反射率是(d,A(I,percent; hkl)):7.01(44; 001),6.46(100; 200,2-bar 01),3.954(30; 201,2 -bar 02),3.236(98; 400、4-bar 02),3.179(33; 041),3.160(38; 022)。该矿物以Anatoliy I. Tsepin(生于1946年)的名字命名,他首先获得了凹凸棒石族矿物的电子微探针数据。类型标本是莫斯科俄罗斯科学院的费斯曼矿物学博物馆。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号