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THE SEDIMENTARY CHARACTERISTICS AND STRUCTURAL EVOLUTION OF THE YOUJIANG COMPOSITE BASIN

Zeng Yunfu, Liu Wenjun, Chen Hongde, Zheng Yongcai, Zhang Jinquan (Chengdu College of Geology, Chengdu, 610059) Li Xiaoquan and Jiang Tingcao (Regional Geological Survey Team of Guangxi, Guilin 541003)  
Situated on the southern margin of South China fold belt, the Youjiang basin has gone through two different development stages. Its outline and structure are closely associated with NW-trending synsedimentary faults. The basin consists of compensative and non-compensative sedimentary facies which form two double-layer structures. The volcanisms in the basin are well developed and are obviously divided into two stages: Hercynian and Indosinian periods. In the Hercynian period, the development of Palaeo-Tethys Ocean made Ailaoshan ocean basin split, which gave rise to a number of NW-trending rift belts in Youjiang area under the conditions of tensile stresses. So, the basin has the characteristics of continental marginal rifts. In the Indosinian period, the conditions of regional stresses were changed. The formation of marginal-Pacific tectonics resulted in much change in the outline and structures of the basin. Meanwhile, the subduction of Ailaoshan ocean basin in the northeast resulted in extension fractures and rifts again in the basin under the new conditions of compressions, and the basin was at the growth stage of back-arc basin. At the end of Indosinian period, the basin was closed.
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