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TECTONICAL EVOLUTION ON THE SOUTHERN MARGIN OF SOUTH CHINA SEA

Yao Bochu  
Here we discuss the topography and geomorpholohy, sedimentary characteristics, distribution of the rigional faults and seismic profiole's characteristics at Wan'an and Zengmu Basins in the Nansha area. Their Cenozoic sediments at Wan'an Basin were subdivided into two tectinical layers. The older, laid in half-grabens of the basement, is terrestrial; The upper is belong to marine facies. The Cenozoic sedi- ment in Zengmu Basin is subdivided into eight regressional sedimentary sequences accordimg to its re- gressional cycles. The NE faults in the Wan'an Basin are en echelon arrangement. The NW faults in the basin have stricke-slip characteristics. We believe that the formation of these basins relate with the sea floor spreading event of the SW Subbasin of South China Sea. The Wan'an Basin is an extensional- shearing basin, Zengmu Basin is a foreland basin.
【CateGory Index】: P736.1
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