头台油田肇261区块沉积微相研究
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摘要
基于岩心观察、地震、测井、录井以及分析化验资料,开展研究区葡萄花油层沉积相特征研究,论述葡萄花油层的沉积相展布及微相类型和特征,建立相应的测井相识别标志。葡萄花油层属于浅水湖泊三角洲沉积,沉积主体以三角洲前缘相带为主,主要沉积微相类型有水下分流河道、席坝、主体砂等。
Based on core observation,seismic,logging,logging and analysis of laboratory data,to carry out the study area Putaohua characteristics of sedimentary facies,to Discuss Putaohua sedimentary facies and microfacies types and characteristics,and establish the corresponding log-phase identification mark.Putaohua are shallow-water lake delta deposition.Deposition of the main delta front facies is mainly.The main types of sedimentary microfacies are Underwater distributary channel,I dam,the main sand,etc..
引文
[1]王建功,王天琦,卫平生,等.大型坳陷湖盆浅水三角洲沉积模式-以松辽盆地北部葡萄花油层为例[J].岩性油气藏,2007,19(2):28-34.
    [2]赵霞飞.动力沉积学与陆相沉积[M].科学出版社(北京),1992.
    [3]刘宗堡,马世忠,吕延防,等.大型凹陷斜坡带油气成藏模式—以三肇凹陷葡萄花油层为例[J].吉林大学学报(地球科学版),2008,38(6):937~945.

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