岩性油气藏
巖性油氣藏
암성유기장
LITHOLOGIC RESERVOIRS
2010年
1期
65-69,75
,共6页
刘琪%李凤杰%郑荣才%刘殿鹤%蒋斌
劉琪%李鳳傑%鄭榮纔%劉殿鶴%蔣斌
류기%리봉걸%정영재%류전학%장빈
高分辨率层序地层%基准面旋回%岩相古地理%上干柴沟组%柴达木盆地
高分辨率層序地層%基準麵鏇迴%巖相古地理%上榦柴溝組%柴達木盆地
고분변솔층서지층%기준면선회%암상고지리%상간시구조%시체목분지
high resolution sequence stratigraphy%base level cycle%lithofacies and paleogeography%upper Ganchaigou Formation%Qaidam Basin
以高分辨率层序地层学原理为指导,通过野外露头剖面、岩心观察、钻井及测井曲线等资料分析,将上干柴沟组划分为2个长期基准面旋回和6个中期基准面旋回,分析了2个级别旋回的结构、叠加样式,在单井层序划分的基础上建立了上干柴沟组层序地层格架对比图.长期基准面旋回结构分布特点与地层之间存在较好的对应关系,位于湖盆中心、地层厚度大的地区主要发育C_2型长期基准面旋回结构,而位于湖盆边部、地层相对较薄的地区主要发育C_1型长期基准面旋回结构.最后以上干柴沟组层序地层等时对比格架为基础,编制了该区的岩相古地理图.
以高分辨率層序地層學原理為指導,通過野外露頭剖麵、巖心觀察、鑽井及測井麯線等資料分析,將上榦柴溝組劃分為2箇長期基準麵鏇迴和6箇中期基準麵鏇迴,分析瞭2箇級彆鏇迴的結構、疊加樣式,在單井層序劃分的基礎上建立瞭上榦柴溝組層序地層格架對比圖.長期基準麵鏇迴結構分佈特點與地層之間存在較好的對應關繫,位于湖盆中心、地層厚度大的地區主要髮育C_2型長期基準麵鏇迴結構,而位于湖盆邊部、地層相對較薄的地區主要髮育C_1型長期基準麵鏇迴結構.最後以上榦柴溝組層序地層等時對比格架為基礎,編製瞭該區的巖相古地理圖.
이고분변솔층서지층학원리위지도,통과야외로두부면、암심관찰、찬정급측정곡선등자료분석,장상간시구조화분위2개장기기준면선회화6개중기기준면선회,분석료2개급별선회적결구、첩가양식,재단정층서화분적기출상건립료상간시구조층서지층격가대비도.장기기준면선회결구분포특점여지층지간존재교호적대응관계,위우호분중심、지층후도대적지구주요발육C_2형장기기준면선회결구,이위우호분변부、지층상대교박적지구주요발육C_1형장기기준면선회결구.최후이상간시구조층서지층등시대비격가위기출,편제료해구적암상고지리도.
Based on high resolution sequence stratigraphy theory,and according to the analysis of description of field outcrop profiles,cores,well drilling and logging trace,the Neogene upper Ganchaigou Formation in west segment,northern margin of Qaidam Basin are divided into two long-term base level cycles and six medium-term base level cycles.The deposition structure and stacking patterns of this two levels cycle are analyzed.Sequence stratigraphic framework of upper Ganchaigou Formation is established based on the sequence division of single well.The distribution feature of long-term base level cycle sequence has better relation with stratum.The long-term base level cycle sequence type of C_2 mainly developed in the central basin and thick stratum areas,and the type of C_1 mainly developed in the margin of the basin and thin stratum areas.Based on the sequence stratigraphic isochronous correlation framework,the lithofacies and paleogeography map of the study area have been drawn up.