摘要
以大牛地气田未开发区( D17井区)太原组2段潮坪沉积为研究对象,基于测井、岩性等特征分析,对潮坪砂坝进行了精细刻画,共识别出了砂坝主体、砂坝侧翼及砂坝侧翼叠置3个沉积微相单元,并建立了沉积微相-岩相-测井相-物性-非均质性-试气成果响应模板。对比结果显示,砂坝主体微相岩性主要为(含砾)石英粗砂岩及岩屑石英砂岩,测井曲线具光滑箱形;砂坝侧翼微相岩性主要为中-细粒砂岩岩屑砂岩、岩屑石英砂岩,测井曲线为齿化箱形、齿化钟形以及漏斗形。根据砂体组合类型,区域上划分出了砂坝主体型砂体带与砂坝侧翼型砂体带。前者砂坝宽度为6~8 km,砂体平均厚度为14.5 m,砂地比平均值为0.53,平均渗透率为0.48×10-3μm2。后者砂坝宽度为4~6 km,砂体平均厚度为10.56 m,砂地比平均值为0.36,平均渗透率为0.36×10-3μm2。砂坝主体型砂体带砂体发育规模大,分布范围广,砂体物性好,中等非均质性,试气成果明显,应作为优先开发的地区。
Logging data and lithological analyses of the tidal-flat depositsin the 2 nd member of the Taiyuan Formation ( D-17 wellblock ) in the Daniudi gas field revealed three sedimentary microfacies:mainsandbar ,sandbar flanking and overlain sandbar flanking-.A response-template of sedimentary micro-facies-lithofacies-logging facies-physical property-heteroge-neity-gas test was also established .Correlation shows that the main sandbar is mainly gravel-bearing quartzose laterite and lithic quartz sandstone , corresponding to smooth-box type logging curves;and thelatter two are mainly medium-to fine-grained lithic sandstone and quartz sandstone , corresponding to dented box-and bell-shaped or funnel-shaped logging curves.Regionally,two belts were identified based on sand body assemblage types:sand body belt consisting main sand-bar and sand body belt consisting sandbar flanking .The former is 6-8 km wide,and has an average thickness of 14.5 m, an average net-to-gross ratio of 0.53 and an average permeability of 0.48 ×10-3μm2 .The latter is 4-6 km wide and has an average thickness of 10.56 m,an average net-to-gross ratio of 0.36 and an average permeability of 0.36 ×10-3μm2 .The former with its well developed and widely distributed sand bodies is considered to be a better development target as it has better physical properties and strong heterogeneity and good gas testing results .
出处
《石油与天然气地质》
EI
CAS
CSCD
北大核心
2015年第2期248-254,共7页
Oil & Gas Geology
基金
国家科技重大专项(2011ZX05007-04-01)
关键词
非均质性
砂坝
潮坪
优质砂体
太原组
大牛地气田
heterogeneity
sand bar
tidal-flat
high-quality sand body
Taiyuan Formation
Daniudi gasfield