Sedimentary evolution of Fuyu Oil layer in 401 block, Sanzhao Depression, Songliao Basin
- DOI
- 10.2991/emcpe-16.2016.67How to use a DOI?
- Keywords
- Songliao Basin, Sanzhao Depression, Fuyu oil layer, sedimentary evolution.
- Abstract
This paper takes Sanzhao Depression in Songliao Basin as the research target. Fuyu oil layer is in the 4th member of Quantou formation, Lower Cretaceous. The target layer in research area is mainly a set of shallow-water delta deposition, experienced the sedimentary evolution process from Delta plain to Delta front, reflect the water level changed from deep to shallow and back to deep. Because of the distributary channel frequently swing, single sand body thin thickness, study of micro facies must be carried out to guide further petroleum development. In the case of lack of core data, this study take advantage of seismic and logging data to analysis the micro facies of each reservoir group and sedimentary evolution of Fuyu oil layer. This paper proposes: 1. F, F, FI3 and FI2 sub-layer of Fuyu oil layer in research area is mainly Delta plain deposition; FI1 sub-layer is mainly Delta front deposition. 2. During the sedimentary period of F, F and FI3 sub-layer, the climate changed from humid to dry, sediment supply gradually increased; During the sedimentary period of FI2 and FI1 sub-layer, the climate changed from dry to humid, sediment supply gradually decreased.
- Copyright
- © 2016, the Authors. Published by Atlantis Press.
- Open Access
- This is an open access article distributed under the CC BY-NC license (http://creativecommons.org/licenses/by-nc/4.0/).
Cite this article
TY - CONF AU - Xin Liu AU - Zhaonian Chen AU - Lei Liu PY - 2016/08 DA - 2016/08 TI - Sedimentary evolution of Fuyu Oil layer in 401 block, Sanzhao Depression, Songliao Basin BT - Proceedings of the 2016 5th International Conference on Environment, Materials, Chemistry and Power Electronics PB - Atlantis Press SP - 316 EP - 321 SN - 2352-5401 UR - https://doi.org/10.2991/emcpe-16.2016.67 DO - 10.2991/emcpe-16.2016.67 ID - Liu2016/08 ER -