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- W1967432674 abstract "One hadean zircon from the Cambrian sandstone in the southern part of South China has a U-Pb age of 4107±29 Ma with ɛ Hf(t) value similar to that of the homochronous depleted mantle and Hf model age of 4102±21 Ma. This demonstrates the existence of hadean crustal remnant in South China. A close match between the U-Pb age and Hf model age with the highly position ɛ Hf(t) value indicates the growth and immediate reworking of juvenile crust from the depleted mantle at ca 4.1 Ga. The prominent “Pan-African” and Grenville zircons derived from the exotic sources were also found in the sample, which indicates a linking between South China and Gondwana in the Cambrian period. The southern part of South China has complex histories of crustal growth and tectonic evolution." @default.
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- W1967432674 date "2012-09-25" @default.
- W1967432674 modified "2023-09-29" @default.
- W1967432674 title "Detrital zircon of 4.1 Ga in South China" @default.
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- W1967432674 doi "https://doi.org/10.1007/s11434-012-5465-8" @default.
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