石英
热液循环
火成岩
分析化学(期刊)
变质岩
杂质
矿物学
地质学
化学
地球化学
色谱法
古生物学
有机化学
地震学
作者
Axel Müller,Monika Koch‐Müller
出处
期刊:Mineralogical Magazine
[The Mineralogical Society]
日期:2009-08-01
卷期号:73 (4): 569-583
被引量:103
标识
DOI:10.1180/minmag.2009.073.4.569
摘要
Abstract Concentrations of a series of trace elements of 14 quartz samples from various geological settings (hydrothermal, igneous, metamorphic) in Norway were determined by LA-ICP-MS. FTIR spectroscopy was applied to the same quartz crystals in order to determine the H concentrations and the speciation of H in the quartz lattice. A refined hypothetical charge neutrality equation is suggested, where the atomic ratio of (Al 3+ + Fe 3+ + B 3+ ) to (P 5+ + H + + Li + + Na + + K + ) should correspond to 1 for natural quartz crystals. The determined concentrations of Al, Fe, B, P, Li, K and OH - species confirm approximately the charge neutrality equation. The high H/(Li+K+P) ion ratio of igneous quartz compared to hydrothermal and metamorphic quartz, suggests that igneous quartz preferentially incorporates H as OH- in lieu of Li, K and P. The results confirm that the FTIR absorption of the OH- band at 3595 cm -1 is attributed to structural B defects in the quartz lattice. The dominating H impurity in most of the quartz samples is, however, molecular H 2 O. The molecular H 2 O is presumably related to waterbearing micro pores and not to visible fluid inclusions, because the spectra were recorded from microscopically clear crystals.
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