SHRIMP single zircon U-Pb dating of the Kongling high-grade metamorphic terrain: Evidence for >3.

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Single zircons from two trondhjemitic gneisses and two clastic metasedimentary rocks without Eu anomaly of the Kongling high-grade metamorphic terrain are dated by the in situ SHRIMP U-Pb method. The results show that the trondhjemitic magma emplaced at 2
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