The formation of the <scp>C</scp>aosiyao giant porphyry <scp>M</scp>o deposit on the northern margin of the <scp>N</scp>orth <scp>C</scp>hina <scp>C</scp>raton: Constraints from <scp>U</scp>―<scp>P</scp>b and <scp>R</scp>e―<scp>O</scp>s geochronology, whole‐rock geochemistry, <scp>H</scp>f isotopes, and oxygen fugacity of the magma
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