Zircon geochronology and Hf isotopes of Mesozoic intrusive rocks from the Yidun terrane, Eastern Tibetan Plateau: Petrogenesis and their bearings with Cu mineralization

• Two main episodes of magmatism at ∼225 Ma and ∼216 Ma occurred in the Yidun terrane.
• Two major episodes of Mesoproterozoic juvenile crust formed in the Yidun terrane.
• The adakitic magma and ore fluids were not resulted from a common magmatic chamber.
• The Mesozoic magmatism and Cu mineralization was related to orogenic collapse.

Zircon U–Pb ages and Hf isotopic composition of Mesozoic intrusive rocks from the Yidun terrane were systematically investigated in order to decipher the geodynamic setting of magmatism and their relationship with Cu-polymetallic mineralization in the Eastern Tibetan Plateau. Zircon U–Pb dating results on seven granitoid rocks and four diorite samples indicate that the Mesozoic plutons from the Yidun terrane were emplaced in the period of 224–214 Ma with a peak at ∼216 Ma. Zircon Hf isotopic compositions show that these intrusive rocks were derived from different source regions. The dioritic porphyries with the formation ages of ∼216 Ma in the Zhongdian area of the southern Yidun terrane, together with the granodiorite of ∼216 Ma from the Maxionggou batholith, originated from the remelting of the late Mesoproterozoic (∼1.2 Ga) juvenile continental lower crust, whereas most granitic rocks were derived from the reworking of the early Mesoproterozoic (∼1.6 to 1.5 Ga) middle-lower crust. Our results, together with previous data, indicate that the collision between the Yidun and Songpan–Ganzi terranes and subsequent orogeny had been completed by the middle Triassic. A post-orogenic collapse model is proposed for the Meosozoic magmatism and related Cu-polymetallic mineralization in the Yidun terrane.