Raman spectroscopy study of the secondary actinolite in gabbrodiorite intrusive rocks from Varan area, Urumieh-Dokhtar Magmatic Arc, Iran

IF 1 Q4 GEOSCIENCES, MULTIDISCIPLINARY
Ghosoun Zheira, B. Rahimzadeh, F. Masoudi
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引用次数: 0

Abstract

Mineralogical studies play a key role in deciphering mineral’s formation and associated geochemical processes in geosciences. This paper presents the application of Raman spectroscopy to the characterization of actinolite in rock samples. The studied actinolite was formed as the pseudomorph of primary pyroxene in gabbrodiorite intrusive rock sample collected from Varan area, Urumieh-Dokhtar Magmatic Arc of Iran. The Raman spectra of micrometer-sized actinolite grains embedded in a crude rock sample are compared with the corresponding literature data for actinolite and tremolite in range of 200-1200 cm-1 and 3600-3700 cm-1 region. The results show that the quantitative estimation of Mg# = Mg/(Mg+Fe2+) can be obtained from the fractional intensities of the OH-stretching bands by applying Raman spectroscopy to micrometer-sized actinolite grains in a crude rough rock sample, which is in good agreement with the results from EMPA. The Raman spectroscopy is a fast method and low-cost for quantitative estimation of Mg# in actinolite.
伊朗乌鲁木齐-多赫塔尔岩浆弧瓦兰地区辉长闪长岩侵入岩中次生放光石的拉曼光谱研究
矿物学研究在地球科学中对矿物的形成和相关的地球化学过程起着关键作用。本文介绍了拉曼光谱在岩石样品中阳起石表征中的应用。所研究的阳起石是在伊朗Urumieh Dokhtar岩浆弧Varan地区采集的辉长岩侵入岩样品中以原生辉石的假晶形式形成的。嵌入粗岩石样品中的微米大小的阳起石颗粒的拉曼光谱与阳起石和透闪石在200-1200cm-1和3600-3700cm-1范围内的相应文献数据进行了比较。结果表明,通过对粗岩石样品中微米尺寸的阳起石颗粒应用拉曼光谱,可以从OH伸缩带的分数强度获得Mg#=Mg/(Mg+Fe2+)的定量估计,这与EMPA的结果非常一致。拉曼光谱法是测定阳起石中Mg#含量的一种快速、低成本的方法。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Iranian Journal of Earth Sciences
Iranian Journal of Earth Sciences GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
1.40
自引率
12.50%
发文量
0
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