首页> 外文期刊>THE CANADIAN MINERALOGIST >ACICULAR ZONED TOURMALINE (MAGNESIO-FOITITE TO FOITITE) FROM A QUARTZ VEIN NEAR TISOVEC, SLOVAKIA: THE RELATIONSHIP BETWEEN CRYSTAL CHEMISTRY AND ACICULAR HABIT
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ACICULAR ZONED TOURMALINE (MAGNESIO-FOITITE TO FOITITE) FROM A QUARTZ VEIN NEAR TISOVEC, SLOVAKIA: THE RELATIONSHIP BETWEEN CRYSTAL CHEMISTRY AND ACICULAR HABIT

机译:斯洛伐克托索维奇附近的一个石英脉状的环状托玛琳(镁橄榄石到橄榄石):晶体化学性质与习惯性行为之间的关系

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摘要

Distinctly chemically zoned tourmaline was found in a quartz vein near Tisovec, Slovak Ore Mountains, Slovakia. The tourmaline forms radial aggregates of light grey to green thin prismatic to acicular crystals growing in cracks in the host rock. The root zone of the aggregates has dravitic to oxy-dravitic compositions, shifting to magnesio-foitite in the middle parts of the crystals and to foititic compositions in the outer parts of the aggregates. The optimized formula, considering the single-crystal structure refinement (SREF) and the chemistry of the magnesio-foititic zone, is similar to(X)(square 0.5Na0.4Ca0.1) (Y)(Mg1.1Al1.0Fe0.82+Fe0.13+) Z(Al5.7Fe0.33+) (Si5.9Al0.1O18) (BO3)(3) (OH)(3) [O-0.6(OH)(0.3)F-0.1], with lattice parameters (SREF) a 15.929(2) angstrom, c 7.163(1) angstrom, and V 1574.0(7) angstrom(3). SREF data as well as a detailed study of bond lengths indicate a dominancy of Al3+ at the Z site substituted by a small proportion of Fe3+, while Fe2+ and Mg2+ essentially occupy the Y site along with a significant amount of Al. The chemical composition is controlled by the substitutions FeMg-1, Al square(Fe, Mg)(-1)Na-1, and AlO(Fe, Mg)(-1)(OH)(-1). The AlO(Fe, Mg)(-1)(OH)(-1) substitution is dominant in the transition from oxy-dravite to magnesio-foitite, and the Al square(Fe, Mg)(-1)Na-1 substitution prevails in the magnesio-foitite and foitite compositions. Both proton-and alkali-deficient substitutions produce the enrichment in Al which can be linked to the forming of the acicular habit. Aluminum strongly prefers the Z-site, whose octahedra form a network of chains parallel to c. Consequently, polymerization of the ZO(6) octahedral network will dominate growth in the a direction. Therefore, the chemical composition, mainly Al enrichment, which is common for most of the acicular to fibrous tourmalines, can be an important factor promoting preferential growth in the c direction. The rate and time for crystallization, which depend mostly on the temperature and cooling rate, are also factors which should be considered.
机译:在斯洛伐克斯洛伐克矿石山的Tisovec附近的石英脉中发现了化学区分明显的电气石。电气石形成放射状的聚集体,从浅灰色到绿色薄的棱柱形到针状晶体生长在宿主岩石的裂缝中。骨料的根部区域具有从德拉威到氧的流变组成,在晶体的中部转移到镁铝辉石,而在骨料的外部则转移到叶绿素。考虑到单晶组织细化(SREF)和镁铁相变区的化学性质,优化公式类似于(X)(平方0.5Na0.4Ca0.1)(Y)(Mg1.1Al1.0Fe0.82 + Fe0.13 +)Z(Al5.7Fe0.33 +)(Si5.9Al0.1O18)(BO3)(3)(OH)(3)[O-0.6(OH)(0.3)F-0.1],晶格参数(SREF)为15.929(2)埃,c 7.163(1)埃和V 1574.0(7)埃(3)。 SREF数据以及对键长的详细研究表明,Z位置的Al3 +占优势,被少量的Fe3 +取代,而Fe2 +和Mg2 +基本上与大量Al一起占据Y位置。化学成分由取代FeMg-1,Al square(Fe,Mg)(-1)Na-1和AlO(Fe,Mg)(-1)(OH)(-1)控制。 AlO(Fe,Mg)(-1)(OH)(-1)取代在从氧-方铅矿到镁橄榄石的过渡过程中占主导地位,并且Al Square(Fe,Mg)(-1)Na-1取代镁镁铝镁橄榄石和铝镁橄榄石组成中占主导地位。质子和碱缺乏的替代都产生Al的富集,这可以与针状习性的形成有关。铝强烈推荐Z部位,其八面体形成与c平行的链状网络。因此,ZO(6)八面体网络的聚合将主导a方向的增长。因此,大多数针状至电气石电气化石中常见的化学成分(主要是铝富集)可能是促进c方向优先生长的重要因素。结晶的速率和时间主要取决于温度和冷却速率,也是应考虑的因素。

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