摘要
东营凹陷王58井区沙四段上亚段纯上5砂组发育了一套含油砂体。为了明确其成因、沉积特征及分布规律,通过分析岩石中碎屑组分类型、结构特征以及沉积地层中的砂砾岩分布、岩石特征元素分布特征等,认为王58井区沙四段上亚段纯上5砂组的砂体是南部和北部2大物源体系共同作用的产物。北部物源控制下的砂体以湖底扇沉积为特征,沉积物粒度粗;南部物源体系控制下的砂体以滑塌浊积扇为特征,沉积物粒度细。
The Chunshang 5th sand group in Es4 of Wang 58 wellblock which is located in the eastern area of Niuzhuang Subsag in Dongying Sag,has a set of oil-bearing sand.According to sand genesis,sedimentary features and distribution,the authors analyzed the rock detrital component types and structural features,sediment distribution and element patterns of sedimentary formations,etc.The sand body of the Chunshang 5th sand group in Es4 of Wang 58 wellblock is the product of interaction between the southern and northern source systems.The sand body under the control of the northern source is characterized by sublacustrine fan sedimentation and rough size of deposition;and the sand body under the control of the southern source is characterized by slumping turbidite fan and fine-sediment deposition.
出处
《油气地质与采收率》
CAS
CSCD
北大核心
2007年第3期38-40,45,共4页
Petroleum Geology and Recovery Efficiency
基金
中国石油天然气股份有限公司科技风险创新研究项目"砂岩岩性圈闭含油性定量评价技术研究"(P05013)的部分成果
关键词
物源方向
砂砾岩
特征元素
东营凹陷
source orientation,glutinite,typical element,Dongying Sag