Detrital zircon record of Neoproterozoic active-margin sedimentation in the eastern Jiangnan Orogen, South China

• Combining U–Pb and Lu–Hf data of detrital zircons from the Neoproterozoic sedimentary rocks to constrain the tectonic evolution of the eastern Jiangnan Orogen.
• The Shuangqiaoshan and Xikou Groups formed in a back-arc to retro-arc foreland basin at ca. 831–815 Ma and ca. 833–817 Ma, respectively.
• The Jiangnan Orogen lasted until ca. 830–815 Ma or even later.
• There was no Grenville (ca. 1000–1300 Ma) juvenile crust in the eastern Yangtze Block.
• The most important generation of juvenile crust occurred at ca. 980–810 Ma.

Precambrian sedimentary sequences in the eastern Jiangnan Orogen, South China, include the Neoproterozoic Shuangqiaoshan and Xikou Groups and the overlying Nanhua Sequence. U–Pb ages of detrital zircons provide tight constraints on the deposition of the Shuangqiaoshan and Xikou Groups at 831–815 Ma and 833–817 Ma, respectively. Rocks from the lower parts of these strata contain dominantly Neoproterozoic detritus with a pronounced age peak at 830–850 Ma, interpreted to be derived from a magmatic arc that has been mostly eroded. This magmatic arc was associated with sedimentation characterized by compositionally immature sediments with dominant early-Neoproterozoic (∼860–810 Ma) zircons that have variable ɛHf(t) values of −21.5 to 14.8. The upper parts of these strata, uncomfortably underlain by the low units, are molasse-type assemblages with additional input of pre-Neoproterozoic detritus, representing sediments accumulated in a retro-arc foreland basin associated with the Jiangnan Orogen.Combining four samples from the Nanhua Sequence, three major magmatic activities at 2.50–2.35 Ga, 2.10–1.90 Ga and 980–810 Ma in the source areas are identified. The older two events are characterized by reworking of pre-existing continental crust. Grenville magmatism and juvenile crust were insignificant in the eastern Jiangnan Orogen. Neoproterozoic zircons reflect generation of juvenile crust at 980–860 Ma, involvement of both juvenile and recycled materials at 860–810 Ma and reworking of pre-existing crust at 805–750 Ma, corresponding to island arc, continental magmatic arc and post-collisional rifting stages in the eastern Jiangnan Orogen.

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