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The Sanchahe quartz monzonite intrusion is situated in the middle segment of the North Qinling tectonic belt, Central China mainland, and consists chiefly of sanukitoid–like and granodioritic‐monzogranitic rocks. The sanukitoid–like rocks are characterized by quartz monzonites, which display higher Mg# (55.0–59.0), and enrichments in Na2O+K2O (7.28–8.94%), Ni (21–2312 ppm), Cr (56–4167 ppm), Sr (553–923...
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