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《GEOLOGICAL SCIENCE AND TECHNOLOGY INFORMATION》 1994-02
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DISCOVERY AND SIGNIFICANCE OF DISCONTINUOUS SEDIMENTARY BEDS IN UPPER PERMIAN HESHAN FORMATIN,GUANGXI PROVINCE

Huang Fengming; Huang Naihe;Wang Gengfa;Tao Jiwen;(China University of Geosciences,Wuhan)Wen Xianduan(China University of Geosciences,Beijing,10083)  
A number of discontinuous sedimentary indexes have been proposed for the first time in the Upper Permian Heshan Formation as follows:(1)brecciated limestones,(2)coarse recrystallization calcite formed by freshwater diagenesis,(3)paleocracks,(4)paleokarst,(5)oxidized crust,(6)conglomerate beds and(7)bedded caves.These indexes are found in the top and in the upper coal seat.At least three discontinuous sedimentations have occurred during the sedimentary process of the Upper Permian Heshan Formation.
【Fund】: 自然科学基金
【CateGory Index】: P618.110.2
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