首页> 美国卫生研究院文献>Data in Brief >Mineral data (SEM electron microprobe Raman spectroscopy) from epithermal hydrothermal alteration of the Miocene Sigri Petrified Forest and host pyroclastic rocks Western Lesbos Greece
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Mineral data (SEM electron microprobe Raman spectroscopy) from epithermal hydrothermal alteration of the Miocene Sigri Petrified Forest and host pyroclastic rocks Western Lesbos Greece

机译:来自中西部中新统西格里石化森林和寄主碎屑岩超热水热蚀变的矿物数据(SEM电子探针拉曼光谱)希腊西部莱斯博斯岛

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摘要

Data available from a detailed mineralogical investigation of the Petrified Forest of Lesbos and its host pyroclastic rocks [1] are summarized and a link is provided to the full data at https://data.mendeley.com/datasets/dxwfd32zms/1. Samples were taken from petrified wood, fresh and devitrified tuffs, and from epithermal veins and epithermally altered tuffs. Backscattered electron (BSE) images were made by scanning electron microscope (SEM) from polished thin sections of 16 samples to show textural relationships between minerals. Minerals were identified by energy dispersive spectroscopy (EDS). Further chemical analysis by electron microprobe (EMP) were made of trace elements in the petrified wood and of Mn-oxide minerals. Polymorphs of silica were investigated by Raman spectroscopy. SEM X-Ray maps were made of selected sites with manganese oxide minerals. In this contribution, the general character of each analyzed sample is summarized and a brief inventory of available data is presented, with specific reference to features in the on-line data. The significance of these data for the origin of the petrification of the wood and the epithermal veining of the host pyroclastic rocks is provided in “Nature of the hydrothermal alteration of the Miocene Sigri Petrified Forest and host pyroclastic rocks, Lesbos, Greece” [1] https://doi.org/10.1016/j.jvolgeores.2018.11.018. The data will be of comparative value to those investigating petrification of wood, devitrification of tuffs, and epithermal Mn-Fe mineralization in other areas.
机译:总结了对莱斯博斯岛石化森林及其宿主热碎屑岩的详细矿物学研究[1]可获得的数据,并在https://data.mendeley.com/datasets/dxwfd32zms/1上提供了完整数据的链接。样品取自木化石,新鲜和失透的凝灰岩,超热脉和超热凝灰岩。通过扫描电子显微镜(SEM)从16个样品的抛光薄片上制成背散射电子(BSE)图像,以显示矿物之间的组织关系。矿物通过能量色散光谱法(EDS)鉴定。用电子探针(EMP)进一步化学分析了木化木材中的微量元素和锰氧化物矿物质。通过拉曼光谱研究了二氧化硅的多晶型物。 SEM X射线图由选定的含有氧化锰矿物的部位制成。在此贡献中,总结了每个分析样本的一般特征,并提供了可用数据的简要清单,并特别参考了在线数据中的功能。这些数据对于木材石化的起源和主体火山碎屑岩的超热脉动的意义在“中新世西格里石化森林和主体火山碎屑岩的热液蚀变性质,希腊莱斯博斯岛”中提供[1]。 https://doi.org/10.1016/j.jvolgeores.2018.11.018。该数据将与研究木材石化,凝灰岩失透以及其他地区超热锰铁矿化的研究具有比较价值。

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