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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2026-04-08 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/14624547/2
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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采用电感耦合等离子体发射光谱仪(ICP-OES)与电感耦合等离子体质谱仪(ICP-MS)完成测定;高亲铁元素丰度与Re-Os同位素组成分别通过高分辨电感耦合等离子体质谱仪(HR-ICP-MS)与负离子热电离质谱仪(N-TIMS)进行分析。本数据集可用于厘定莱斯沃斯蛇绿岩套橄榄岩的构造亲缘性,明确其形成环境为洋陆过渡环境。
提供机构:
Guochen Dong; D. Graham Pearson; Dongxu Li; YONG XU; Jingao Liu
创建时间:
2021-05-20
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