4.7 Article

Solubility of corundum in the system Al2O3-SiO2-H2O-NaCl at 800 °C and 10 kbar

期刊

CHEMICAL GEOLOGY
卷 249, 期 3-4, 页码 250-261

出版社

ELSEVIER
DOI: 10.1016/j.chemgeo.2008.01.002

关键词

corundum solubility; experimental petrology; Al mobility; metamorphic fluids

向作者/读者索取更多资源

The solubility of corundum was measured at 800 degrees C and 10 kbar in NaCl-H2O-SiO2 fluids over NaCl mole fractions (X-NaCl) of 0 to 0.5 and SiO2 concentrations of zero to quartz or albite+melt saturation, depending on X-NaCl. Experiments were performed in apiston-cylinder apparatus. Dissolved Al2O3 and SiO2 were determined by weight losses of corundum and quartz crystals, or by bulk compositions of bracketing experiments. Although kyanite and sillimanite are slightly more stable than corundum+quartz at these pressures (P) and temperatures (7), neither appeared in any of the experiments. Results indicate that the enhancement of corundum solubility by NaCl at this P and T is further promoted by the addition of SiO2. At quartz saturation, significant enhancement occurs in initially pure H2O and addition of NaCl yields yet higher Al2O3 concentrations. At 0.03 <= X-NaCl <= 0.1, quartz saturation is replaced by albite+silicate melt. The anhydrous melt composition is nearly on the join NaAlSi3O8-SiO2. Al2O3 molality rises rapidly with NaCl concentration to 0.038 at X-NaCl = 0.1 and then increases more slowly to 0.052 at halite saturation. There is, in addition, a measurable reciprocal enhancement of Si solubility by virtue of dissolved Al at a fixed X-NaCl. Quench pH in NaCl-bearing fluids is strongly acidic and Na/Cl <1 in quench solutes, suggesting low pH at high P and T These observations, combined with previous work indicating Si-Al and Na-Al complexing, lead to the hypothesis that the reciprocal solubility enhancement of Al and Si is due to formation of Na-aluminosilicate complexes. Mass balance consideration suggests that the bulk Si/Al ratio of the group of complexes ranges from 1 to 2 in the NaCl-free system, to >3 at high X-NaCl. Our data show that Al2O3 is a moderately soluble component in quartz+ aluminosilicate-saturated rocks in the presence of intergranular salt solutions at deep-crustal metamorphic P-T conditions and commonly realized salinities. Al2O3 should not be regarded as a fixed reference component, because it may exhibit substantial mobility. (C) 2008 Elsevier B.V. All rights reserved.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.7
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据