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《Geology and Mineral Resources of South China》 2007-01
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Discovery of the Permian in the Danzhou-Tunchang Area of Hainan Island and its Geological Significance

LONG Wen-guo1,2,TONG Jin-nan2,ZHU Yao-he1,ZHOU Jin-bo1,LI Sun-xiong1,SHI Chun1(1.Hainan Geological Survey,Haikou 570226 Hainan,China;2.Faculty of Earth Science,China University of geosciences,Wuhan,430074 Hubei China)  
Fossiles,shuch as Radiolaria etc.,were collected from the strata assigned previously to the Carboniferous in the area of Danzhou-Tunchang in central Hainan.Now the age of the strata has been determined to be Early-Mid Permian which divided into two parts.The lower part formed in a littoral-epeiric environment,is a series of clastic rocks,partly contains carbonate rock and metamorphic basic volcanic rocks and the upper part formed in a bathypelagic environment is a series of sediments with chert,partly contains metamorphic basic volcanic rocks.In comparision with the Early-Mid Permian strata exposed widely in the western and western-southern Hainan island,there are appreciable difference in the features of the lithologic association,sediment type,fossil concentration and generic and species components,as well as the geological setting.The determination of this sequence of strata has great significance for the study of the sedimentary facies of the Early-Mid Permian strata and reconstruction of the paleogeographic environment in Hainan and the study of the stratigraphic evolution in the Palaeotethyan tectonic development stage and tectonic setting of the basin in Hainan and its adjacent areas.
【Fund】: 中国地质调查局1:25万琼海县幅区调(200113000041)资助
【CateGory Index】: P534.46
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