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Bulk-rock Major and Trace Element Compositions, Highly Siderophile Element Abundances and Re-Os Isotopic Compositions of the Lesvos Ophiolitic Peridotites

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Figshare2021-05-20 更新2026-04-28 收录
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https://figshare.com/articles/dataset/Bulk-rock_Major_and_Trace_Element_Compositions_Highly_Siderophile_Element_Abundances_and_Re-Os_Isotopic_Compositions_of_the_Lesvos_Ophiolitic_Peridotites/14624547
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Bulk-rock major and trace element compositions are determined by ICP-OES and ICP-MS, respectively; Highly siderophile element abundances and Re-Os isotopic compositions are analyzed by HR-ICP-MS and N-TIMS, respectively.This dataset can help to identify the tectonic affinity of the Lesvos ophiolitic peridotites as ocean-continent-transition environment.

全岩主量元素与微量元素组成分别通过电感耦合等离子体发射光谱法(ICP-OES)与电感耦合等离子体质谱法(ICP-MS)测定;高亲铁元素丰度与铼-锇同位素组成分别通过高分辨电感耦合等离子体质谱法(HR-ICP-MS)与负离子热表面电离质谱法(N-TIMS)分析。本数据集可用于判别莱斯沃斯蛇绿岩套橄榄岩的构造亲缘性,其形成环境为洋陆过渡带。
创建时间:
2021-05-20
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