沉积与特提斯地质2016，Vol.36Issue(3)：83-90,8.
高邮凹陷北斜坡戴二段辫状河三角洲沉积特征和演化
Sedimentary characteristics and evolution of the braided delta deposits in the second member of the Dainan Formation in northern Gaoyou depression,Jiangsu
摘要
Abstract
In the light of core examination,well logs,laboratory data and seismic data,the type,distribution and evolution of sedimentary facies are dealt with for the braided delta deposits in the second member of the Dainan Formation in northern Gaoyou depression,Jiangsu. The second member of the Dainan Formation is dominated by the braided delta facies,followed by the meandering and lake facies. The braided delta facies in the study area may be subdivided into the delta plain subfacies including the braided channel and overbank microfacies,delta front subfacies including the subaqueous distributary channel,subaqueous interdistributary bay,channel mouth bar, distal bar and sheet sands microfacies,and prodelta subfacies including the prodelta mud microfacies. The distribution and evolution of the sedimentary facies and genetic mechanism of the braided delta are examined in detail in this study.关键词
辫状河三角洲/沉积演化/高邮凹陷/戴二段Key words
braided delta/sedimentary evolution/Gaoyou depression/second member of the Dainan Formation分类
能源科技引用本文复制引用
李坤,董桂玉,张振国,邱永峰,毕天卓,张丽春..高邮凹陷北斜坡戴二段辫状河三角洲沉积特征和演化[J].沉积与特提斯地质,2016,36(3):83-90,8.基金项目
河北省自然科学基金（D2013209045）、河北省科技计划项目 （）
