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《Acta Geological Sinica》 1990-01
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THE LATE PROTEROZOIC TRENCH-BASIN-ARC SYSTEM IN NORTHEASTERN JIANGXI-SOUTHERN ANHUI PROVINCES

Xu Bei (Department of Geosciences, Nanjing University)  
The late Proterozoic can be divided into three rock sequences in northeastern Jiangxi and southern Anhui provinces which represent three palaeogeographic units.The first sequence is called the Dengshan Group which is distributed from northeastern Jiangxi to western Zhejiang, comprising a volcanic series with an isotopic age of 818 Ma 122 samples illustrate a continuous change in chemical composition and, particularly, andesite is an important part in the volcanic series. In Pearce's and Wood's diagrams the majority of the volcanic rocks show an affinity to island arc. So the Dengshan Group might occur in an island arc belt.The second is called the Shangxi Group, which is represented by turbidite distributed from northeastern Jiangxi to southern Anhui. A lot of turbidite facies strata have been recognized, which may be divided into two turbidite facies associations. Association Ⅰ, lying in the north includes D, C and G facies, and association 11, B_2 and C facies, lying in the south. It is cleer that associations Ⅰ and Ⅱ reflect respectively the outer-and inner-fan positions, by which a northward developing turbidite fan is recognized in a backarc basin.The third sequence, called the Qigong Group or Tieshajie Group, crops out along the railway form Jiangxi to Zhejiang, comprising carbonate, argillaceous, siliceous and volcanic rocks. It is regarded as a trench and fore-are formation.According to the above-mentioned analysis, a late Proterozoic trench-arc basin system can be reconstructed.
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