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《成都地质学院学报》 1989-04
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THE TECTONIC FRAMEWORK AND THE EVOLUTION OF LITHOFACIES AND PALEOGEOGRAPHY OF DEVONIAN IN EASTERN YUNNAN AND SOUTHWESTERN GUIZHOU

Zheng Rongcai;Zhang Jinquan  
Eastern Yunnan and Southwestern Guizhou were located on the eastern fringe of the Ancient Tethys Sea during De- vonian period. The tectonic framework in those areas could be divided into three different tectonic units, i. e. Ailaoshan oceaic rift system belonging to the Tethys plate, Southeastern Yunnan and Southern Guishou passive continental margin rift system and Northeastern Yunnan and Wesern Guizhou inner continental rift system belonging to Yangzi plate. The three sedimentary basins differing in tectonic nature and inner-framework, were developed in the three rift systems re- spectively. The late paleozoic sedimentary formation and volcanic activity of the basins were controlled by the expanding and strike-slip movement of syndepositional faults developed in the three basins. The pattern of sedimentary facies distri- bution and evolution of lithofacies and paleogeography of Devonian in each basin were concordant with the syndeposi- tional fault activity in eacn rift system.
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