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摘要:
Based on comprehensive analysis of core,cast thin section,logging and seismic data,the sedimentary and reservoir architectures of the MB 1-2 sub-member of Mishrif Formation in Halfaya Oilfield,Iraq,are studied.The MB 1-2 sub-member of Mishrif Formation has three types of microfacies,lagoon,bioclastic shoal,and tidal channel,and facies architecture controlled by sequence stratigraphy.In the 4th-order sequence,the lagoon facies aggradated vertically,and the bioclastic shoals in lenticular shape embed in the background of lagoon,the end of the sequence is incised by the"meandering river"shape tide channel,which represents the depositional discontinuity.Three types of reservoirs including tidal channel grainstone to packstone reservoirs,bioclastic shoal grainstone to packstone reservoirs and dissolved lagoon wackestone reservoirs are developed.The reservoir architectures within tidal channel and bioclastic shoal are strickly controlled by grainy facies,whereas the dissolved lagoon reservoirs controlled by both facies and dissolution are related to the sequence boundary.The reservoir sections occur mainly in the 4 th sequence highstand systems tract(HST)and are separated by barriers formed in the transgressive systems tract(TST).Complicated facies architecture and dissolution modification resulted in strong heterogeneity within the reservoir,which showed the characteristics of"attic type"architecture.The results of this study can guide the development of similar reservoirs in the Middle East.
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篇名 Sedimentary and reservoir architectures of MB1-2 sub-member of Middle Cretaceous Mishrif Formation of Halfaya Oilfield in Iraq
来源期刊 石油勘探与开发:英文版 学科 工学
关键词 Iraq Halfaya Oilfield CRETACEOUS Mishrif Formation sedimentary microfacies reservoir architecture
年,卷(期) 2020,(4) 所属期刊栏目
研究方向 页码范围 762-772
页数 11页 分类号 TE31
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研究主题发展历程
节点文献
Iraq
Halfaya
Oilfield
CRETACEOUS
Mishrif
Formation
sedimentary
microfacies
reservoir
architecture
研究起点
研究来源
研究分支
研究去脉
引文网络交叉学科
相关学者/机构
期刊影响力
石油勘探与开发:英文版
双月刊
2096-4803
10-1529/TE
北京市海淀区学院路20号
80-232
出版文献量(篇)
331
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0
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