<b>Data for "Evolution of the subcontinental lithospheric mantle beneath </b><b>the Xing’an Mongolia accretionary orogenic belt</b><b>: implications for the stabilization of cratons"</b>

This file includes Supplementary Tables S1 to S4 for the publication "Evolution of the subcontinental lithospheric mantle beneath the Xing'an Mongolia accretionary orogenic belt: implications for the stabilization of cratons" (submitted to Earth-Science Reviews in May 2024).<br>Table S1. Petrography, major element compositions, equilibrium temperatures, and densities of xenoliths.<br>Table S2. Mineral major element compositions.<br>Table S3. Whole-rock HSE abundances and Re-Os isotope compositions.<br>Table S4. Mineral trace element concentrations.本文件包含2024年5月提交至《地球科学评论》的论文《兴蒙增生造山带之下大陆下岩石圈地幔（subcontinental lithospheric mantle）的演化：对克拉通稳定作用的启示》的补充表S1至S4。 表S1：捕虏体的岩石学特征、主量元素组成、平衡温度及密度。 表S2：矿物主量元素组成。 表S3：全岩高亲铁元素（high-siderophile elements, HSE）丰度与Re-Os同位素组成。 表S4：矿物微量元素浓度。