Zircon U–Pb Ages and Geochemistry of Granite Porphyries in the Yangla Cu Deposit, SW China: Constraints on Petrogenesis and Tectonic Evolution of the Jinshajiang Suture Belt

<div>The underground tunnel 3,250 m section map of the Yangla copper deposit, Yunnan, China. 1: Devonian (Linong Formation); 2: Devonian (Jiangbian Formation); 3: granitic porphyry; 4: copper ore body; 5: fault and corresponding number; 6: fracture zone; 7: geological boundary line; and 8: tunnel and corresponding number.</div>

Geofluids

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Figure 4: Zircon U–Pb Ages and Geochemistry of Granite Porphyries in the Yangla Cu Deposit, SW China: Constraints on Petrogenesis and Tectonic Evolution of the Jinshajiang Suture Belt 

Figure 4 | Zircon U–Pb Ages and Geochemistry of Granite Porphyries in the Yangla Cu Deposit, SW China: Constraints on Petrogenesis and Tectonic Evolution of the Jinshajiang Suture Belt 