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>Composition diagrams of the granite porphyry and granodiorite. The area between the high-pressure (12-15 kbar) and low-pressure (≤5 kbar) curves encompasses the range of depths at which mantle-crust interaction takes place (After Douce, 1999 [<a href="/journals/geofluids/2020/8852277/#B82">82</a>]).</div>

Geofluids

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Figure 22

Figure 22: 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 22 | 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 