Detrital zircon of 4.1 Ga in South China

作者: YaJun Xu , YuanSheng Du , HongWei Huang , ZhiQiang Huang , LiSha Hu

DOI: 10.1007/S11434-012-5465-8

关键词: South chinaPaleontologyMantle (geology)TectonicsCrustGondwanaHadeanGeochemistryZirconGeology

摘要: One hadean zircon from the Cambrian sandstone in southern part of South China has a U-Pb age 4107±29 Ma with ɛ Hf(t) value similar to that homochronous depleted mantle and Hf model 4102±21 Ma. This demonstrates existence crustal remnant China. A close match between highly position indicates growth immediate reworking juvenile crust at ca 4.1 Ga. The prominent “Pan-African” Grenville zircons derived exotic sources were also found sample, which linking Gondwana period. complex histories tectonic evolution.

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