摘要
在层序地层研究基础上 ,结合右江盆地油气勘探成果 ,建立了右江盆地层序地层格架与油气生储盖组合之间的关系模型。具体是以南盘江凹陷及十万大山地区为重点 ,通过泥盆纪—中三叠世层序地层中生储盖组合的研究 ,阐述相应的不同级别层序格架 (二级及三级 )中储集体的成因类型及时空分布规律 。
Based on the sequence stratigraphy, in conjunction with the result of petroleum exploration, the correlation model of sequence stratigraphic framework and oil & gas source\|reservoir\|cap rock association has been established. Emphasized on Nanpanjiang depression and Shiwandashan basin, this paper deals with the genetic type and distribution pattern of source\|reservoir\|cap rock strata within different hierarchies of sequence stratigraphic frameworks in the Youjiang Basin, and then discusses on their genesis and development model. Various sequence frameworks in different genetic basins contain different hydrocarbon prospects. In general, transgressive system tracts (TST), condensed section (CS), highstand system tracts (HST) and lowstand system tracts (LST) of interplatform basin, deep\|water basin are generally important source rocks and significant cap rocks,and coal\|bearing carbonate formations of highstand system tract in cratonic basin and carbonate platform . Highstand system tracts and lowstand system tracts in cratonic basin and carbonate platform are important reservoins,and karst reservoir is developped along sequence boundary.Reservoirs maimly include all kinds of favourable sandbodies within different system tracts:①basin floor and slope fans, delta front, alluvial fan, channel sandbodies, progradation complex, shoal\|bioherm\|reef complex, calcareous and mixed clastic turbidites within lowstand system tract; ②sandbodies of barrier beach, shoal, estuary, tide\|controlled delta, fandelta, turbidity fan, lag sediment, bioherm\|reef complex, pyroclast turbidite within transgressiue system tract; ③river and wave dominated deltatic sandbodies, alluvial\|fan\|channel sandbodies, fandelta, turbidity fan, terrigenous and carbonate shales, bioherm\|reef complex, calcareous\|clastic beach\|bioherm\|reef complex, calcareous clastic turbidite and dolostone within highstand system tract; and ④paleokarst reservoir dominated by sequence boundary.
出处
《沉积学报》
CAS
CSCD
北大核心
2000年第2期215-220,共6页
Acta Sedimentologica Sinica
