<b>Data for "Evolution of the subcontinental lithospheric mantle beneath </b><b>accretionary orogens</b><b>: implications for the stabilization of cratons"</b>

This file includes Supplementary Tables S1 to S5 for the publication "Evolution of the subcontinental lithospheric mantle beneath accretionary orogens: implications for the stabilization of cratons" (submitted to Earth and Planetary Science Letters in July 2024).<br>Table S1. Petrography, major element compositions, pressure-temperature, 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.Table S5. WR major element compositions, pressure-temperature, lithospheric thickness in references本文件包含2024年7月投稿至《地球与行星科学通讯》的论文《增生造山带下大陆岩石圈地幔演化：对克拉通稳定的启示》的补充表S1至S5。<br>表S1：捕虏体的岩石学、主量元素组成、温压条件及密度<br>表S2：矿物主量元素组成<br>表S3：全岩高亲铁元素（Highly Siderophile Elements）丰度及Re-Os同位素组成<br>表S4：矿物微量元素浓度<br>表S5：全岩主量元素组成、温压条件及参考文献中的岩石圈厚度