Data for: Origin of high-Cr chromite deposits in nascent mantle wedges: Petrological and geochemical constraints from the Neo-Tethyan Luobusa ophiolite, Tibet

The uploaded tables above are supplementary to our manuscript, titled "Origin of high-Cr chromite deposits in nascent mantle wedges: Petrological and geochemical constraints from the Neo-Tethyan Luobusa ophiolite, Tibet". Table-S1 presents the EPMA data of chromite obtained in this study. Table-S2 presents the complied major element compositions of clinopyroxene in peridotites and chromitites from previous studies. Table-S3 presents the complied REE compositions of clinopyroxene in the cpx-rich and cpx-poor harzburgites from previous studies. Table-S4 presents the complied REE compositions of harzburgites and dunites from previous studies. Table-S5 presents the calculated REE compositions of the parental melts of clinopyroxene grains in the Luobusa harzburgites. Detailed sources of the complied data have been given in the Table-S2 to Table-S5.

上文上传的表格为本篇题为《新生地幔楔中高铬铬铁矿矿床的成因：来自西藏新特提斯罗萨蛇绿岩的岩石学与地球化学约束》的论文手稿提供补充数据。表S1展示了本研究中获得的铬铁矿电子探针显微分析（EPMA）数据。表S2汇总了前人研究中橄榄岩及铬铁矿体中单斜辉石的主量元素组成。表S3汇总了前人研究中富单斜辉石及贫单斜辉石方辉橄榄岩的单斜辉石稀土元素（REE）组成。表S4汇总了前人研究中方辉橄榄岩与纯橄榄岩的稀土元素（REE）组成。表S5计算得到了罗萨蛇绿岩方辉橄榄岩中单斜辉石颗粒的母熔浆稀土元素（REE）组成。上述汇总数据的详细来源已在表S2至表S5中列明。