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.

上述上传的表格系本论文之补充，论文题目为《新生地幔楔中高铬铬铁矿床的起源：来自青藏高原新特提斯卢布斯阿乌尔橄榄岩的岩石学和地球化学限制》，其中表-S1展示了本研究获得铬铁矿的电子探针显微分析（EPMA）数据。表-S2展示了先前研究中橄榄岩和铬铁矿中斜方辉石的主要元素组成的综合数据。表-S3展示了先前研究中富含cpx和贫cpx的哈巴格塔橄榄岩中斜方辉石的稀土元素（REE）组成的综合数据。表-S4展示了先前研究中哈巴格塔橄榄岩和辉长岩的稀土元素组成的综合数据。表-S5展示了卢布斯阿乌尔哈巴格塔橄榄岩中斜方辉石晶粒的母岩浆的稀土元素组成的计算数据。综合数据的详细来源已列于表-S2至表-S5。