土耳其Şenkaya绿铜矿矿物学、岩石学和地球化学特征

IF 1.3 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Hami̇t Haluk Seli̇m, Aykut Güçtekin, Ferhan Şahi̇n, Mustafa Kaya, Beri̇l Kaya, Elanur Güner, K. Taş, Ahmet Karakaş, Yasemi̇n Kantarçeken
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引用次数: 0

摘要

:Şenkaya chrysoprase是一种宝石,可以在土耳其安纳托利亚东北部隆起的Kırdağ的Şenka ya(Erzurum)县西北偏西的Turnalı村附近找到。Chrysoprase是一种在Örükyayla Mélange发现的浅深绿色隐晶质结构宝石,仅在Şenkaya县发现,在土耳其商业上以相同的名称为人所知。从现场采集样品,用于确定Şenkaya chrysoprase的矿物学岩石学、XRD、XRF、ICP-MS、光学阴极发光显微镜(OCLM)、FTIR拉曼光谱和稳定同位素特性。根据矿物学和岩石学检查,Şenkaya chrysoprase在宏观尺度上具有普遍的不均匀颜色分布,并且具有5 Mohs矿物硬度。在以蛇纹石为主要成分、部分块状蛋白石型二氧化硅的微检查中发现了微石英填充(10%-15%)。XRF分析表明,许多样品具有高的SiO2值(wt%)。作为微量元素、稀土元素、使用ICP-MS的Au-Pt组分析的结果,Ni(167–387 ppm)和Co(12.57–74.78 ppm)的值非常显著。在OCLM研究中,由于一些微量活化元素,很少观察到能产生CL并能以不同颜色传播CL的金属矿物。三个温石棉样品的氧同位素(δ18OV-SMOW)值分别为24.8‰、27.7‰和30.63‰,平均形成温度为96–99°C。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Mineralogical, petrological, and geochemical characteristics of Şenkaya Chrysoprase,Turkey
: Şenkaya chrysoprase is a gemstone and can be found near the Turnalı village located in the west-northwest of Şenkaya (Erzurum) county in the uplifted Kırdağ of Northeast Anatolia of Turkey. Chrysoprase only found in Şenkaya County and known with the same name commercially in Turkey is a light-dark green and cryptocrystalline structure gemstone encountered in the Örükyayla Mélange. Samples were collected from the field for defining mineralogical-petrographical, XRD, XRF, ICP-MS, optical cathodoluminescence microscopy (OCLM), FTIR-Raman and stable isotopic properties of Şenkaya chrysoprase. According to mineralogical and petrographic examination, Şenkaya chrysoprase has generally heterogeneous color distribution in macroscale and has 5 Mohs mineral hardness. Microquartz filling (10%–15%) was seen in the microexamination with serpentine as main component with partly massive opal type silica. The XRF analyses indicate that many samples had high SiO 2 values wt%). As a result of trace elements, rare earth elements, Au-Pt group analyses using ICP-MS, Ni (167–387 ppm) and Co (12.57–74.78 ppm) values are quite remarkable. In the OCLM studies, few metallic minerals which could produce CL and could spread CL in different colors due to some trace activator elements were observed. Oxygen isotopic (δ 18 O V-SMOW ) values obtained from three chrysoprase samples are 24.8‰, 27.7‰ and 30.63‰, respectively and mean formation temperature is 96–99 o C.
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来源期刊
Turkish Journal of Earth Sciences
Turkish Journal of Earth Sciences 地学-地球科学综合
CiteScore
2.40
自引率
10.00%
发文量
6
审稿时长
6 months
期刊介绍: The Turkish Journal of Earth Sciences is published electronically 6 times a year by the Scientific and Technological Research Council of Turkey (TÜBİTAK). It is an international English-language journal for the publication of significant original recent research in a wide spectrum of topics in the earth sciences, such as geology, structural geology, tectonics, sedimentology, geochemistry, geochronology, paleontology, igneous and metamorphic petrology, mineralogy, biostratigraphy, geophysics, geomorphology, paleoecology and oceanography, and mineral deposits. Contribution is open to researchers of all nationalities.
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