Middle Neoproterozoic sedimentary strata are widely distributed on the periphery of Yangtze Block. In western Jiangnan Orogen, they divided into Lengjiaxi and Banxi groups by “Wuling unconformity,” Group is further Madiyi Formation Wuqiangxi “Xihuangshan unconformity.” However, timing tectonic significance Wuling Xihuangshan unconformities remain unclear, which hampers our understanding Precamb...