<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 S4 for the publication "Evolution of the subcontinental lithospheric mantle beneath accretionary orogens: implications for the stabilization of cratons" (submitted to Geochimica et Cosmochimica Acta 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《地球化学与宇宙化学学报》（Geochimica et Cosmochimica Acta）的论文《增生造山带下大陆岩石圈地幔的演化：对克拉通稳定的启示》的补充表S1至S4。<br>表S1 捕虏体（xenoliths）的岩石学、主量元素组成、平衡温度与密度<br>表S2 矿物主量元素组成<br>表S3 全岩高亲铁元素（Highly Siderophile Elements，HSE）丰度与Re-Os同位素组成<br>表S4 矿物微量元素浓度

搜集汇总

背景与挑战

背景概述

该数据集为地球化学研究提供支持，包含四个Excel表格，涵盖捕虏体的岩相学、主微量元素组成、同位素数据等，用于分析增生造山带下大陆岩石圈地幔的演化及其对克拉通稳定化的影响。数据集关联一篇提交至《Geochimica et Cosmochimica Acta》的学术论文，适用于同位素地球化学和地质年代学领域的研究。