U-Pb age and Hf isotope composition of detrital zircons from Neoproterozoic sedimentary units in southern Anhui Province, South China: Implications for the provenance, tectonic evolution and glacial history of the eastern Jiangnan Orogen
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文摘

Sediments were sourced from the Jiangnan Orogen and northern Yangtze Block.

Zircon Hf isotopes record a switch from subduction to collision at 860 Ma.

A regional unconformity was developed along the Jiangnan Orogen at 830–800 Ma.

The Leigongwu diamictite in the Lantian section is a single Marinoan-age glacial unit.

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