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SEQUENCE STRATIGRAPHY OF PERMIAN REEFS, YOU JIANG BASIN,SOUTHWEST CHINA

Qin Jianxiong Zeng Yunfu Cheng Hongde Tian Jiangchun (Institute of Sedimentology,Chengdu University of Technology,Chengdu\ 610059)  
An exhaustive study and related sequence stratigraphic model for Permian reef in the Youjiand Basin has been established in this paper.This model suggests that reef develops at every stage during sea level cycle and possesses all kinds of sequence internal architecture and genetic framework.LST reef characterized by ag gradational bioherm or patch reef,is generally associated with mixed clastic turbidite,siliceous limestone and mudstone.SMT reef,larger in size and relatively much in amount compared to LST reef,develops within inter-platform basin and slope because of better hydrodynamic environment during SMT;During transgression interplatform basin bioberm-reef complex continuously or discontinuously retrogrades towards ba sin margin and slope and then internal platform,and finally brings about fransgr assive bioherm-reef compler overlapping from basin to platform,including interpl atform-basin reef,slope reef,platform-edge reef and internal platform reefwith reefal top characterized by hardground,biodisturbation surface,submarine welded surface,flooding surface and give-up surface etc.Reef cap includes siliceous rock,pyroclastic turbidite,radiomite,deep trace facies,biocondensed bed,plankton-facies limestone etc.HST reef characterized by a great quantity of offlappinga ggradation-progradation-compoundreef association,including barrier reef,table reef,horeseshoe reef,atoll,and bioberm reef with various vertical and lateral zonation.Reefal top includes subaerial surface,paleocarstic surface,erosion surface,caliche and dolostone cap etc.Reefal cap mainly includes eluvial facies,tidalfacies,turbidites and bioberm-beach facies etc.
【CateGory Index】: P534.46
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