Geochronological analysis reveals the carboniferous rifting and basin development in north-central Inner Mongolia, indicating significant geological evolution.
Mineral chemical, geochronological, whole-rock elemental and Sr-Nd isotopic, and zircon Hf-O isotopic compositions (Tables S1–S5) for the early Carboniferous diabase-granite complex from the Wulagai region of north-central Inner Mongolia. Representative element and element ratio variation diagrams for Wulagai diabase and granites (Figures S1–S3). Detailed descriptions of analytical methods (Text S1).
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Yang et al. (2025) studied this question.
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