Petrogenesis of the Tongcun adakitic intrusive complex in non-arc settings was discussed.
New age for late Cu mineralization and Pb isotope of the Tongcun complex, molybdenite and chalcopyrite were analyzed.
9915">The genesis of the porphyry Mo–Cu deposit associated with the Tongcun adakitic complex was discussed.
9995">A new simplified genetic model is given for the formation of the Tongcun Middle-Late Jurassic I–type granites.