陆相盆地水下扇扇中亚相的微相细分——以东营凹陷史南地区沙二9梁家楼水下扇为例

The division to microfacies in middle-fan of subaqueous fan in continental basin: a case study from Liangjialou subaqueous fan in Shinan area of the Dongying sag

  • 摘要: 通过对东营凹陷史南地区沙二9砂层组的小层精细对比和微相细分,可以将梁家楼水下扇扇中亚相进一步划分出辫状水道、辫状砂坝、“边滩”、侧缘砂坝、侧缘分支沟道、末端砂坝、冲溢扇、低阶地、高阶地等9个微相。不同微相之间的砂体粒度变化、平面发育位置都有明显的不同,尤其是其中的辫状砂坝、“边滩”、侧缘砂坝是在水下地形较平坦,坡度较小的情况下,由辫状沟道侧向迁移形成的。对水下扇扇中亚相的微相细分和重新厘定,不仅有助于对水下扇沉积过程的进一步了解,而且也将有助于油田对水下扇砂体剩余油的分布研究和开发方案的调整。

     

    Abstract: Based on elaborate correlation to substratum of Es29 sand group in Shinan area, Dongying sag,the middle-fan of Liangjialou subaqueous fan can be divided in 9 micro-facieses: braided channel, braided bar, "point bar", lateral bar, lateral branching channel, end bar of branching channel, washover fan, low slope, high slope. There are obviously differences in changes of sand-grain-size and plane distribution among these microfacieses, the formation of braided bar, "point bar" and lateral bar were derived from lateral migration of braided channel with little gradient and flatter subaqueous landform. The elaborate division to microfacieses can help us to realize deposition of subaqueous fan and the distribution of remaining oil, and adjust the development plan to oil field.

     

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