...
首页> 外文期刊>Mineralogy and Petrology >Zincoberaunite, ZnFe53+(PO4)(4)(OH)(5)center dot 6H(2)O, a new mineral from the Hagendorf South pegmatite, Germany
【24h】

Zincoberaunite, ZnFe53+(PO4)(4)(OH)(5)center dot 6H(2)O, a new mineral from the Hagendorf South pegmatite, Germany

机译:Zincoberaunite,Znfe53 +(PO4)(4)(OH)(5)中心点6H(2)o,来自德国Hagendorf South Pegmatite的新矿物质

获取原文
获取原文并翻译 | 示例

摘要

The new mineral zincoberaunite, ideally ZnFe3+ (5)(PO4)(4)(OH)(5)center dot 6H(2)O, the Zn analogue of beraunite, is found in the Hagendorf South granitic pegmatite, Hagendorf, Bavaria, Germany, in two associations: (1) with potassium feldspar, quartz, jungite, phosphophyllite and mitridatite (the holotype) and (2) with flurlite, plimerite, Zn-bearing beraunite, schoonerite, parascholzite/scholzite, robertsite and altered phosphophyllite (the cotype). Zincoberaunite occurs as radial or randomly oriented aggregates of flexible fibers up to 1.5 mm long and up to 3 mu m thick. D (calc) is 2.92 g/cm(3) for the holotype and 2.94 g/cm(3) for the cotype. Zincoberaunite is optically biaxial (-), alpha = 1.745(5), beta = 1.760(5), gamma = 1.770(5), 2V (meas) = 80(5)A degrees. Chemical composition of the holotype (electron probe microanalyser; H2O by gas chromatography of ignition products) is: MgO 0.28 wt%, CaO 0.47 wt%, ZnO 7.36 wt%, Al2O3 0.88 wt%, Fe2O3 42.42 wt%, P2O5 31.63 wt%, H2O 16.2 wt%, total 101.1 wt%. The empirical formula calculated on the basis of 27 oxygen atoms per formula unit is (Zn0.83Ca0.08Mg0.06)(a0.97)(Fe3+ Al-4.88(0.16))(Sigma 5.04)(PO4)(4.09)(OH)(4.78) center dot 5.86H(2)O. Zincoberaunite is monoclinic, space group C2/c; refined unit cell parameters (for the holotype at room temperature and the cotype at 100 K, respectively) are: a 20.837(2) and 20.836(4), b 5.1624(4) and 5.148(1), c 19.250(1) and 19.228(4) , angstrom,beta 93.252(5) and 93.21(3)degrees, V 2067.3(3) and 2059.2(7) angstrom(3), Z = 4. The crystal structure of the holotype specimen has been refined by the Rietveld method (R (p) = 0.30 %; R (B) = 0.18 %) whereas the structure of the cotype has been solved from the single crystal data and refined to R (1) = 0.056 based on 1900 unique reflections with I > 2 sigma(I). The strongest reflections of the powder X-ray diffraction pattern of the holotype specimen [(d, ) (I, %) (hkl)] are: 10.37 (100) (200), 9.58 (32) (002), 7.24 (26) (20-2), 4.817 (22) (111), 4.409 (13) (112), 3.483 (14) (11-4, 600), 3.431 (14) (404), 3.194 (15) (006, 31-4), 3.079 (33) (314).
机译:新的矿物锌杂志,理想情况下,ZnFe3 +(5)(PO4)(4)(OH)(5)中心点6H(2)O是Beraunite的Zn模拟,在Hagendorf South Gracingitic Pegmatite,Hagendorf,Bavaria,德国,在两个关联中:(1)用钾长石,石英,jungite,磷酸丝体和丙磷酸盐(全磷灰石)和(2),用氟钨酸盐,韧带,Zn的Beraunite,Schoonerite,Parascholzite / Scholit,Robertsite和改变的磷酸磷光酯(奇型) )。锌诺贝拉石作为径向或随机取向的柔性纤维的聚集体,柔性纤维长达1.5毫米,厚度高达3亩。 D(CAPC)为奇特类型为2.92g / cm(3),为奇型为2.94g / cm(3)。锌诺贝尼石是光学双轴( - ),α= 1.745(5),β= 1.760(5),γ= 1.770(5),2V(MEAS)= 80(5)度。全型化学成分(电子探针微晶体;用点火产品的气相色谱法)是:MgO 0.28wt%,CaO 0.47wt%,ZnO 7.36wt%,Al 2 O 3 0.88wt%,Fe 2 O 3 42.42wt%,P2O5 31.63wt%, H2O 16.2重量%,总101.1重量%。根据每配方单元27个氧原子计算的经验公式是(Zn0.83ca0.08mg0.06)(A0.97)(Fe3 + Al-4.88(0.16))(Sigma 5.04)(PO4)(4.09)(哦)(4.78)中心点5.86H(2)o。锌诺贝里岩是单斜延长的,空间组C2 / C;精细的单位细胞参数(用于在室温下的全型和100 k的奇型)是:20.837(2)和20.836(4),B 5.1624(4)和5.148(1),C 19.250(1)和19.228(4),Angstrom,Beta 93.252(5)和93.21(3)度,V 2067.3(3)和2059.2(7)埃(3),Z = 4.全型试样的晶体结构已被精制RIETVELD方法(R(P)= 0.30%; R(b)= 0.18%),奇特的结构已从单晶数据中解决并基于1900次独特的I>基于1900个独特的反射来精制R(1)= 0.056 2个西格玛(i)。全型样品[(d,)(I,%)(HK1)的粉末X射线衍射图案的最强反射为:10.37(100)(200),9.58(32)(002),7.24(26 )(20-2),4.817(22)(111),4.409(13)(112),3.483(14)(11-4,600),3.431(14)(404),3.194(15)(006, 31-4),3.079(33)(314)。

著录项

相似文献

  • 外文文献
  • 中文文献
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