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.

本数据集包含0.5吉帕斯卡（GPa）、800~1200摄氏度条件下碳酸盐分解及熔体-碳酸盐（含铁方解石至白云石）相互作用实验的主量元素矿物与玻璃组分分析数据，其研究意义在于揭示中地壳压力下钙-镁-铁碳酸盐体系中脱碳作用(Decarbonation)随温度的变化规律，以及该体系与弧岩浆的同化作用机制，并为长期气候研究提供理论启示。