Major element analysis of carbonate thermal decomposition and melt-carbonate (calcite to dolomite) interaction experiments

Major element mineral and glass analysis of carbonate decomposition and melt-carbonate (Fe-bearing calcite to dolomite) interaction experiments at 0.5 GPa, 800–1200°C with implications for Decarbonation in the Ca-Mg-Fe carbonate system at mid-crustal pressure as a function of temperature and assimilation with arc magmas–Implications for long-term climate.

本数据集涵盖0.5吉帕斯卡（GPa）、800–1200℃条件下碳酸盐分解及熔体-（含铁方解石（Fe-bearing calcite）至白云石（dolomite））碳酸盐相互作用实验的主要元素矿物与玻璃相分析数据。该数据集可为中地壳压力（mid-crustal pressure）下钙-镁-铁碳酸盐体系（Ca-Mg-Fe carbonate system）内随温度变化的脱碳作用（Decarbonation）规律及其与弧岩浆（arc magmas）的同化作用机制提供实验支撑，同时对探讨长期气候变化（long-term climate）具有重要启示价值。