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On the lower boundary of the Shuangqiaoshan Group in Jiangxi


, : On the lower boundary of the Shuangqiaoshan Group in Jiangxi. Regional Geology of China = Zhongquo Quyu Dizhi 16(4): 410-414

Based on gravel composition, fabrics and regional distribution of the metaconglomerate coupled with the marked difference in metamorphism and deformation of the upper part (Shuangqiaoshan Group) and lower part (Xingzi Group complex) of the suite, the author suggests that the metaconglomerate should be assigned to the base of the Shuangqiaoshan Group. It is evidence of the unconformity between the Middle Proterozoic Shuangqiaoshan Group and the underlying Lower Proterozoic Xingzi Group complex. Owing to the influence of tectonic superimposition and late-stage reworking, both show faults or hidden unconformable contact relationships at present.

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