摘要
将伊洛瓦底盆地始新统沉积相划分为冲积扇陆相沉积相、浪控三角洲沉积相、河口湾海陆过渡沉积相和无障壁海岸等海相沉积相。在此基础上,了解始新统各地层的沉积相分布情况和整个沉积相演化过程,总结该盆地始新统沉积相的主要沉积模式——浅海陆棚沉积模式和冲积扇—浪控三角洲沉积模式。最后,综合评价该盆地始新统有利勘探区域。
The article divides the facies into alluvial fan continental facies,wave-controlled delta facies,estuary paralic facies and non-barrier coast facies,which is marine facies.Based on it,the facies distribution and evolution of each formation on Eocene Series is clarified,and the primary deposition pattern for facies of the petroliferous basin is summarized as the shallow marine shelf and wave-controlled delta-alluvial deposition pattern.Finally,the advantaged exploration region on Eocene Series in the basin can be evaluated synthetically.
出处
《重庆科技学院学报(自然科学版)》
CAS
2013年第2期111-114,118,共5页
Journal of Chongqing University of Science and Technology:Natural Sciences Edition
基金
中石化集团国际石油勘探开发有限公司项目(GKKY-10-40)
关键词
伊洛瓦底盆地
始新统
沉积相
沉积演化
沉积模式
有利区域
Irrawaddy Basin
Eocene
sedimentary facies
sedimentary evolution
sedimentation model
favorable area