Supplemental Material: Carbon-rich polyphasic inclusions in postcollisional mafic magmatic rocks from the Dabie Shan, China: Implications for the carbon cycle in continental subduction zones

Figure S1: Microphotographs display the textures of polyphasic inclusions trapped in the olivine of Zhujiapu rocks from Dabie Shan. Figure S2: Microphotographs show the abundant carbon phases inside both types of inclusions in four host minerals of Zhujiapu rocks from Dabie Shan. Figure S3: The variation of δ²⁶Mg versus δ²⁵Mg for Zhujiapu rocks from Dabie Shan aligns along the terrestrial equilibrium mass fractionation line.