首页> 外文期刊>Neues Jahrbuch fur Mineralogie, Abhandlungen >Substitution mechanism in tourmalines of the 'fluor-elbaite'-rossmanite series from Wolkenburg, Saxony, Germany
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Substitution mechanism in tourmalines of the 'fluor-elbaite'-rossmanite series from Wolkenburg, Saxony, Germany

机译:来自德国萨克森州沃尔肯堡的“氟-伊贝石”-罗斯曼石系列电气石的替代机理

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Single-crystal structure and chemical (EMPA, SIMS, TGA) data were obtained from three pale coloured to colourless Al- and Li-rich tourmaline crystals from a pegmatite from Wolkenburg near Limbach-Oberfrohna, Saxony, Germany. Tourmaline samples of the "fluor-elbaite"-rossmanite solid solution series were chemically (including the light elements) and structurally characterized for the first time. The crystal chemical formulae of these three investigated samples range from a "fluor-elbaite" dominant composition with ~X(Na_(0.65)square_(0.29)Ca_(0.06))~Y(Al_(1.64)Li_(1.12)Mn_(0.10)~(2+)Fe_(0.02)~(2+)square_(0.12)~ZAl_6(BO_3O_3(Si_(5.90)B_(0.10))O_(18)(OH)_3[F_(0.72)(OH)_(0.18)O_(0.10)], over ~X(Na_(0.54)square_(0.45)Ca_(0.01))~Y(Al_(1.90)Li_(0.97)Mn_(0.03)~(2+)Fe~(2+)square_(0.09))~ZAl_6 (BO_3)_3~T(Si_(5.82)B_(0.18))O_(18)~V(OH)_3~W[(OH)_(0.51)F_(.37)O_(0.12)] to Na-rich rossmanite with the composition ~X(square_(0.51)Na_(0.48)Ca(0.01))~Y(Al_(2.02)Li_(0.71)Mn_(0.03)~(2+)square_(0.24))~Z(Al_6(BO_3)_3~T(Si_(5.69)Al_(0.17)B_(0.14))O_(18)~V(OH)_3~W[(OH)_(0.70)F_(0.26)O_(0.04]When the rossmanite component increases, while the "fluor-elbaite" component decreases, the olenite component also increases. In a pegmatitic system where essentially no Fe, Mn, Ti and Mg are available, the Li content is an important factor, which seems to control the amount of Si in tourmaline. Once the Li~(1+) content is lower, Al~(3+) cations (with a higher oxidation /tate) must occupy the Y site. For a charge-balanced formula, other cation sites must therefore have lower bulk charges. This can be achieved by increasing vacancies at the X site and increasing amounts of trivalent cations at the T site. In the Wolkenburg tourmalines of the "fluor-elbaite"-rossmanite series both substitutions are observed. For our investigated tourmalines we can propose a modified (coupled) Tschermaks' substitution with ~Xsquare + ~YAl~(3+) + ~T(A1, B)~(3+)<->~XNa~+ + ~YLi~+ + ~TSi~(4+). The F content is dependent on the charge of the X-site occupants. There is also a good negative correlation between the charge of the X-site occupants and the X-02 distance, which can be used to draw some conclusions about the X-site occupancy when only single-crystal structure data are available.
机译:单晶结构和化学数据(EMPA,SIMS,TGA)是从德国萨克森州Limbach-Oberfrohna附近的Wolkenburg的伟晶岩中的三种浅色至无色富含Al和Li的电气石晶体获得的。首次对“氟-elbaite” -rossmanite固溶体系列的电气石样品进行了化学分析(包括轻元素)并对其结构进行了表征。这三个研究样品的晶体化学分子式为〜(X(Na_(0.65)square_(0.29)Ca_(0.06))〜Y(Al_(1.64)Li_(1.12)Mn_(0.10) )〜(2+)Fe_(0.02)〜(2+)square_(0.12)〜ZAl_6(BO_3O_3(Si_(5.90)B_(0.10))O_(18)(OH)_3 [F_(0.72)(OH)_ (0.18)O_(0.10)] ~~(X(Na_(0.54)square_(0.45)Ca_(0.01))〜Y(Al_(1.90)Li_(0.97)Mn_(0.03)〜(2+)Fe〜(2 +)square_(0.09))〜ZAl_6(BO_3)_3〜T(Si_(5.82)B_(0.18))O_(18)〜V(OH)_3〜W [(OH)_(0.51)F _(。37) O_(0.12)]到组成为〜X(square_(0.51)Na_(0.48)Ca(0.01))〜Y(Al_(2.02)Li_(0.71)Mn_(0.03)〜(2+)square_ (0.24))〜Z(Al_6(BO_3)_3〜T(Si_(5.69)Al_(0.17)B_(0.14))O_(18)〜V(OH)_3〜W [(OH)_(0.70)F_( 0.26)O_(0.04)当rossmanite组分增加而“ fluor-elbaite”组分减少时,olenite组分也增加。在基本上没有Fe,Mn,Ti和Mg的聚晶体系中,Li含量为一个重要的因素,它似乎控制着电气石中的Si含量,一旦Li〜(1+)含量较低时,Al〜(3+)阳离子(氧化率较高)必须占据Y位。因此,对于电荷平衡的公式,其他阳离子位点必须具有较低的总体电荷。这可以通过增加X位点的空位和增加T位点的三价阳离子的量来实现。在“氟-elbaite” -rossmanite系列的Wolkenburg电气石中,观察到两个取代。对于我们研究的电气石,我们可以用〜Xsquare +〜YAl〜(3+)+〜T(A1,B)〜(3 +)<->〜XNa〜+ +〜YLi〜 + +〜TSi〜(4+)。 F含量取决于X部位乘员的电荷。 X位置乘员的电荷与X-02距离之间也存在良好的负相关关系,当只有单晶结构数据可用时,可以用来得出有关X位置乘积的一些结论。

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