首页> 外文期刊>Mineralogical Magazine >New minerals with a modular structure derived from hatrurite from the pyrometamorphic Hatrurim Complex. Part II. Zadovite, BaCa6[(SiO4)(PO4)](PO4)(2)F and aradite, BaCa6[(SiO4)(VO4)](VO4)(2)F, from paralavas of the Hatrurim Basin, Negev Desert, Israel
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New minerals with a modular structure derived from hatrurite from the pyrometamorphic Hatrurim Complex. Part II. Zadovite, BaCa6[(SiO4)(PO4)](PO4)(2)F and aradite, BaCa6[(SiO4)(VO4)](VO4)(2)F, from paralavas of the Hatrurim Basin, Negev Desert, Israel

机译:源自焦亚晶型Hatrurim配合物的白云母具有模块化结构的新矿物。第二部分Zadovite BaCa6 [(SiO4)(PO4)](PO4)(2)F,并从以色列内盖夫沙漠Hatrurim盆地的巴拉瓦斯烧掉BaCa6 [(SiO4)(VO4)](VO4)(2)F

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Zadovite, BaCa6[(SiO4)(PO4)](PO4)(2)F (R (3) over bar m, a = 7.0966(1) angstrom, c = 25.7284(3), V = 1122.13(3) angstrom(3), Z = 3) and aradite, BaCa6[(SiO4)(VO4)] (VO4)(2)F (R (3) over bar m, a = 7.1300(1), c = 26.2033(9) angstrom, V = 1153.63(6) angstrom(3), Z = 3) are two new mineral species of a novel modular structure type related closely to the structure of nabimusaite, KCa12(SiO4)(4)(SO4)(2)O2F. Both minerals occur in paralavas enclosed in pyrometamorphic rocks of the Hatrurim Complex, Negev desert, Israel. Zadovite and aradite are colourless, transparent with a white streak, have a vitreous lustre and an uneven fracture. Both minerals are uniaxial (-) with refractive indices (589 nm) omega = 1.711(2), epsilon = 1.708(2) (zadovite) and omega = 1.784(3), epsilon = 1.780(3) (aradite). The zadovite structure type comprises two tetrahedral sites, which may host a broad compositional range of atoms such as Si, P, V and S. Results of electron microprobe analyses show a correlation between excess Si4+ and S6+ contents, suggesting the substitution scheme 2(P,V)(5+) = Si4+ + S6+ at the tetrahedral sites. This points to the possibility of new minerals isostructural with zadovite with end-member formulae BaCa6(SiO4)(2)[(VO4)(SO4)]F, BaCa6(SiO4)(1.5)[(SO4)(0.5)](PO4)(2)]F and BaCa6[(SiO4)(1.5)(SO4)(0.5)](VO4)(2)F. The Raman spectra of aradite and zadovite reflect the varying PO4 (e.g. change of band intensity at similar to 1031 cm(-1)) and VO4 contents (e.g. change of band intensity at similar to 835 cm(-1)). The presence of SO4 leads to an additional Raman band at similar to 997 cm(-1). The structure of zadovite-series minerals belonging to the nabimusaite group is characterized by a 1:1 alternation of antiperovskite-like {[FCa6](TO4)(2)}(4+) modules and Ba(TO4)(2-)(4) modules.
机译:Zadovite,BaCa6 [(SiO4)(PO4)](PO4)(2)F(R(3)在bar m上,a = 7.0966(1)埃,c = 25.7284(3),V = 1122.13(3)埃( 3),Z = 3)并放出,BaCa6 [(SiO4)(VO4)](VO4)(2)F(R(3)在bar m上,a = 7.1300(1),c = 26.2033(9)埃, V = 1153.63(6)埃(3),Z = 3)是两种新的矿物种类,它们是一种新颖的模块化结构类型,与na石(KCa12(SiO4)(4)(SO4)(2)O2F)的结构密切相关。两种矿物都发生在以色列内盖夫沙漠哈特里姆综合体的亚变质岩中的巴拉瓦斯中。 Zadovite和aradite无色透明,带有白色条纹,具有玻璃光泽和不均匀断裂。两种矿物均为单轴(-),折射率(589 nm)的Omega = 1.711(2),ε= 1.708(2)(zadovite)和omega = 1.784(3),epsilon = 1.780(3)(aradite)。闪锌矿结构类型包括两个四面体位点,这些位点可能具有较宽的组成范围,例如Si,P,V和S。原子电子探针分析的结果表明,过量的Si4 +和S6 +含量之间存在相关性,表明取代方案2(P ,V)(5+)=四面体位点处的Si4 + + S6 +。这指出了新的矿物可能具有以端基分子式BaCa6(SiO4)(2)[(VO4)(SO4)] F,BaCa6(SiO4)(1.5)[(SO4)(0.5)](PO4 )(2)] F和BaCa6 [(SiO4)(1.5)(SO4)(0.5)](VO4)(2)F。芳铁矿和钙钛矿的拉曼光谱反映了不断变化的PO4(例如,类似于1031 cm(-1)的能带强度的变化)和VO4含量(例如类似于835 cm(-1)的能带强度的变化)。 SO4的存在会导致一个额外的拉曼光谱带,类似于997 cm(-1)。属于纳比亚辉石类的锌闪石系列矿物的结构特征是:抗钙钛矿状{[FCa6](TO4)(2)}(4+)模和Ba(TO4)(2-)( 4)模块。

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