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ID:9235089
大小:2.66 MB
页数:9页
时间:2018-04-24
《上扬子北缘震旦纪_早古生代沉积演化与储层分布特征》由会员上传分享,免费在线阅读,更多相关内容在行业资料-天天文库。
1、1000-0569/2011/027(03)-0672-80ActaPetrologicaSinica岩石学报上扬子北缘震旦纪-早古生代沉积演化与*储层分布特征余谦牟传龙张海全谭钦银许效松闫剑飞YUQian,MUChuanLong,ZHANGHaiQuan,TANQinYin,XUXiaoSongandYANJianFei成都地质矿产研究所,成都610082ChengduInstituteofGeologyandMineralResources,Chengdu610082,China2010-1
2、0-20收稿,2011-01-30改回.YuQ,MuCL,ZhangHQ,TanQY,XuXSandYanJF.2011.SedimentaryevolutionandreservoirdistributionofnorthernUpperYangtzeplateinSinian-EarlyPaleozoic.ActaPetrologicaSinica,27(3):672-680AbstractThesedimentaryevolutionofthenorthernUpperYangtzepla
3、teisaffectedbySouthQinlingstructureonthenorth,Longmenshanstructureonthewest,andalsolong-terminheritedupliftofHannanpaleocontinentonthenorth.InSinian-EarlyPaleozoicwithQinlingSeaonthenorth,BayanHarSeaonthewest,itssedimentaryfillingevolutionisdifferent
4、fromNEedgeofYangtzeplate.Ontopofvolcanic-sedimentaryrockofTiechuanshanFormation-XixiangFormationandtilliteofNanhuaSystem,mainlyunderwentcarbonateplatforminSinian,shelfinEarly-MiddleCambrian,carbonateplatformandpericratonicupliftinLateCambrian-EarlyOr
5、dovician,platformsdrowninginMiddleOrdovician,andshelfdepositioninLateOrdovician-EarlySilurian.Somesetsofregionalsourcerockandfavorablereservoirareformedinthesedimentaryevolution.Thereservoirmainlyincludealgalreef-dolomitereservoirofDenigyingFormation
6、,ooliticlimestonereservoirofXiannvdongFormation,sandreservoirofCanglangpuFormation,anddolomitereservoirofShilongdongFormation.Thereservoirdistributeswidely.Althoughdominatedbylowporosityandlowpermeabilityoverall,carbonatitereservoirinsomeareasdevelop
7、scorrosionandthepermeabilityisfavorable.TheDingyingFormationandShilongdongFormationarethemainreservoirandpotentialexplorationtargetinnorthernYangtzeplate,inwhichoilandgasexplorationpotentialisconsiderable.KeywordsNorthernYangtzePlate;Sinian;EarlyPale
8、ozoic;Sedimentaryevolution;Reservoirdistribution摘要上扬子北缘地层沉积演化既受北部南秦岭构造、西部龙门山构造、同时也受北部汉南古陆的长期继承性隆起影响。震旦纪-早古生代,其北部为秦岭洋、西部为巴颜喀拉洋,沉积充填演化序列有别于扬子地台东南边缘。在铁船山组-西乡组火山-沉积岩系和南华系冰碛岩之上,主要经历了震旦纪初始碳酸盐台地、早中寒武世陆棚、晚末寒武世-早奥陶世碳酸盐台地及克拉通边缘隆升、中晚奥陶世台地淹没、晚奥陶-早志留世滞留陆棚沉积等阶段。沉积
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