| 胡状集油田沙三~3亚段浊积岩沉积特征 |
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| 引用本文： | 赖伟庆,张金亮.胡状集油田沙三~3亚段浊积岩沉积特征[J].西安石油大学学报(自然科学版),1996(2). |
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| 作者姓名： | 赖伟庆 张金亮 |
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| 作者单位： | 西安石油学院石油天然气地质研究所 |
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| 摘 要： | 胡状集油田沙三~３亚段浊积岩除了发育鲍马层序外，还发育有各种准同生变形构造、槽模、大型交错层理、浪成沙纹层理和深水遗迹化石．该浊积岩复合体为一浊积扇体系，水道浊积岩由砾质和砂质高密度浊流沉积序列组成，而非水道浊积岩则主要由经典浊积岩组成．
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| 关 键 词： | 浊积岩，交错层理，遗迹化石，胡状集油田，东濮凹陷，鲍马层序 |
Sedimentary Features of Turbidites in the Third Submember of Shahejie Formation,Huzhuangji Oil Field |
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| Lai weiqing et al.Sedimentary Features of Turbidites in the Third Submember of Shahejie Formation,Huzhuangji Oil Field[J].Journal of Xian Shiyou University,1996(2). |
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| Authors: | Lai weiqing |
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| Abstract: | esides developing Bouma sequence, the turbidite in the third submember of Shahejie formation,Huzhuangji Oil Field developed various parasyngennetic deformed structures,flute casts,large scale cross beddings, wave ripple cross beddings and deep water trace fossils.The turbidite complex body belongs to a turbid fan system. The channel turbidite is composed of high density gravel and sand sequence. The non-channel turbidite consists of classic turbidites with Bouma sequence. |
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| Keywords: | turbidite cross bedding trace fossil/[Huzhuangji Oil Field Dongpu depression Bouma sequence] |
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