渤海湾盆地黄河口凹陷古近系东营组三段沉积特征
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摘要
综合利用地震、测井、录井、岩心及分析化验资料,通过综合分析和系统沉积学编图,确定了黄河口凹陷古近系东营组三段(东三段)主要发育扇三角洲、辫状河三角洲、湖泊和湖底扇。东三段下部辫状河三角洲发育于黄河口凹陷的西南部和南部,在渤南凸起的南北两侧均发育扇三角洲朵体,半深湖—深湖主要分布于西部深凹部位,在B-2断隆带南部的半深湖区发育湖底扇,绝大部分地带为滨浅湖沉积,以滨浅湖泥滩和混合滩沉积为主。东三段上部辫状河三角洲发育于黄河口凹陷的西南部、南部及D-4断隆带的南侧,仅在渤南凸起的北侧发育扇三角洲朵体,半深湖—深湖主要分布于西北次凹部位,绝大部分地带为滨浅湖沉积,以滨浅湖泥滩和混合滩沉积为主。E-1-1—F-4-1井一带继承性发育滨浅湖砂质滩坝沉积。滨浅湖砂质滩坝由含砾粗砂岩、含砾中砂岩、含砾细砂岩及中、细砂岩组成,骨架颗粒成分以石英为主,发育低角度交错层理,纹层由定向排列的砾石或暗色组分显示,纹层平直,以低角度相交。滨浅湖砂质滩坝微相区为东三段优质储集层发育区。
Based on the comprehensive analyses of seismic,wireline log and drilling data,core and analytical and testing results,integrated analyses have been carried out on the sedimentary facies of the Member 3 of Paleogene Dongying Formation and the sedimentary facies maps have been compiled.The lower part of Member 3 of Dongying Formation is dominated by fan delta,braided fluvial delta,lacustrine and sublacustrine fan facies.The braided fluvial delta of the lower part of Member 3 of Dongying Formation was developed in southwestern and northern areas of the Huanghekou Sag.The fan delta was developed in the south and north sides of the Bonan uplift.The semi-deep to deep lake was developed in the western deep sagging area and the sublacustrine fan in the semi-deep lake south of the B-2 faulted uplift belt and most areas were dominated by shore-shallow lacustrine facies including shore-shallow lacustrine muddy bank and mixed bank.During the deposition of the upper part of Member 3 of Dongying Formation,braided fluvial delta facies was developed and mainly distributed in the southwestern and southern parts of the sag and the southern side of the D-4 faulted uplift belt,fan delta was limited to the northern side of the Bonan uplift,and semi-deep to deep lacustrine facies was developed in the western deep sagging area which was dominated by shore-shallow lacustrine facies.The sandy beach bar was developed in the E-1-1 —F-4-1 well area.The sandy beach bar is composed of gravelly coarse sandstones,gravelly medium grained sandstones and medium-fine grained sandstones with the detrital grains being dominated by quartz.Low angle cross bedding was developed.The shore-shallow lacustrine sandy beach bar microfacies is the favorable facies belt for high quality reservoir development.
Based on the comprehensive analyses of seismic,wireline log and drilling data,core and analytical and testing results,integrated analyses have been carried out on the sedimentary facies of the Member 3 of Paleogene Dongying Formation and the sedimentary facies maps have been compiled.The lower part of Member 3 of Dongying Formation is dominated by fan delta,braided fluvial delta,lacustrine and sublacustrine fan facies.The braided fluvial delta of the lower part of Member 3 of Dongying Formation was developed in southwestern and northern areas of the Huanghekou Sag.The fan delta was developed in the south and north sides of the Bonan uplift.The semi-deep to deep lake was developed in the western deep sagging area and the sublacustrine fan in the semi-deep lake south of the B-2 faulted uplift belt and most areas were dominated by shore-shallow lacustrine facies including shore-shallow lacustrine muddy bank and mixed bank.During the deposition of the upper part of Member 3 of Dongying Formation,braided fluvial delta facies was developed and mainly distributed in the southwestern and southern parts of the sag and the southern side of the D-4 faulted uplift belt,fan delta was limited to the northern side of the Bonan uplift,and semi-deep to deep lacustrine facies was developed in the western deep sagging area which was dominated by shore-shallow lacustrine facies.The sandy beach bar was developed in the E-1-1 —F-4-1 well area.The sandy beach bar is composed of gravelly coarse sandstones,gravelly medium grained sandstones and medium-fine grained sandstones with the detrital grains being dominated by quartz.Low angle cross bedding was developed.The shore-shallow lacustrine sandy beach bar microfacies is the favorable facies belt for high quality reservoir development.
引文
蔡东升,罗毓晖,武文来,等.2001.渤海浅层构造变形特征、成因机理与渤中坳陷及其周围油气富集的关系[J].中国海上油气(地质),15(1):35-43.
陈世悦,杨剑萍,操应长.2000.惠民凹陷西部下第三系沙河街组两种滩坝沉积特征[J].煤田地质与勘探,28(3):1-4.
崔周旗,李文厚,李莉,等.2005.冀中饶阳凹陷蠡县斜坡古近系沙河街组沙二段及沙一段下亚段沉积相与隐蔽油藏[J].古地理学报,7(3):373-381.
邓运华.1999.渤海湾盆地凹陷-凸起油气聚集的差异性[J].中国海上油气(地质),13(6):401-405.
郝芳.2005.超压盆地生烃作用动力学与油气成藏机理[M].北京科学出版社,287-300.
侯贵廷,钱祥麟,宋新民.1998.渤海湾盆地形成机制研究[J].北京大学学报(自然科学版),34(4):503-509.
徐长贵,许效松,丘东洲,等.2005.辽东湾地区辽西凹陷中南部古系构造格架与层序地层格架及古地理分析[J].古地理学报7(4):449-459.
张金亮,侯杨善,赖伟庆.1996.南马庄油田沙三段储集层特征[J].西安石油学院学报,11(2):8-14.
朱筱敏,信荃麟,张晋仁.1994.断陷湖盆滩坝储集体沉积特征及沉积模式[J].沉积学报,12(2):20-28.
Cai Dongsheng,Luo Yuhui,Wu Wenlai,et al.2001.Shallowtectonic de-formation and its relationship to hydrocarbon enrichment in BozhongDepression and adjacent areas,Bohai Bay Basin[J].China OffshoreOil and Gas(Geology),15(1):35-43(in Chinese with English ab-stract).
Chen Shiyue,Yang Jianping,Cao Yingchang.2000.Sedimentary charac-teristics of two kinds of beach-bars of Oligocene Shahejie Formationin western Huimin Depression,China[J].Coal Geology&Explora-tion,28(3):1-4(in Chinese with English abstract).
Cui Zhouqi,Li Wenhou,Li Li,et al.2005.Sedimentary facies and subtlepetroleum reservoir of the Member2and lower Submember of Mem-ber1of Shahejie Formation of Paleogene on Lixian Slope of RaoyangSag,Central Hebei Province[J].Journal of Palaeogeography,7(3):373-381(in Chinese with English abstract).
Deng Yunhua.1999.Analysing the petroleum accumulational differenceof sag and uplift in Bohai Bay Basin[J].China Offshore Oil andGas(Geology),13(6):401-405(in Chinese with English ab-stract).
Hao Fang.2005.Kinetics of Hydrocarbon Generation and Mechanisms ofPetroleum Accumulation in Overpressured Basins[M].Beijing:Sci-ence Press,287-300(in Chinese).
Hou Guiting,Qian Xianglin,Song Xinmin.1998.The origin of the BohaiBay Basin[J].Acta Scientiarum Naturalium(Universitatis Pekinen-sis),34(4):503-509(in Chinese with English abstract).
Xu Changgui,Xu Xiaosong,Qiu Dongzhou,et al.2005.Structural andsequence stratigraphic frameworks and palaeogeography of the Paleo-gene in central-southern Liaoxi Sag,Liaodongwan Bay area[J].Journal of Palaeogeography,7(4):449-459(in Chinese with Eng-lish abstract).
Zhang Jinliang,Hou Yangshan,Lai Weiqing.1996.Reservoir character-istics of the Third Member of Shahejie Formation in NanmazhuangOilfield[J].Journal of Xi an Petroleum Institute,11(2):8-14(inChinese with English abstract).
Zhu Xiaomin,Xin Quanlin,Zhang Jinren.1994.Sedimentary characteris-tics and models of the beach-bar reservoirs in faulted down lacustrinebasins[J].Acta Sedimentologica Sinica,12(2):20-28(in Chi-nese with English abstract).
陈世悦,杨剑萍,操应长.2000.惠民凹陷西部下第三系沙河街组两种滩坝沉积特征[J].煤田地质与勘探,28(3):1-4.
崔周旗,李文厚,李莉,等.2005.冀中饶阳凹陷蠡县斜坡古近系沙河街组沙二段及沙一段下亚段沉积相与隐蔽油藏[J].古地理学报,7(3):373-381.
邓运华.1999.渤海湾盆地凹陷-凸起油气聚集的差异性[J].中国海上油气(地质),13(6):401-405.
郝芳.2005.超压盆地生烃作用动力学与油气成藏机理[M].北京科学出版社,287-300.
侯贵廷,钱祥麟,宋新民.1998.渤海湾盆地形成机制研究[J].北京大学学报(自然科学版),34(4):503-509.
徐长贵,许效松,丘东洲,等.2005.辽东湾地区辽西凹陷中南部古系构造格架与层序地层格架及古地理分析[J].古地理学报7(4):449-459.
张金亮,侯杨善,赖伟庆.1996.南马庄油田沙三段储集层特征[J].西安石油学院学报,11(2):8-14.
朱筱敏,信荃麟,张晋仁.1994.断陷湖盆滩坝储集体沉积特征及沉积模式[J].沉积学报,12(2):20-28.
Cai Dongsheng,Luo Yuhui,Wu Wenlai,et al.2001.Shallowtectonic de-formation and its relationship to hydrocarbon enrichment in BozhongDepression and adjacent areas,Bohai Bay Basin[J].China OffshoreOil and Gas(Geology),15(1):35-43(in Chinese with English ab-stract).
Chen Shiyue,Yang Jianping,Cao Yingchang.2000.Sedimentary charac-teristics of two kinds of beach-bars of Oligocene Shahejie Formationin western Huimin Depression,China[J].Coal Geology&Explora-tion,28(3):1-4(in Chinese with English abstract).
Cui Zhouqi,Li Wenhou,Li Li,et al.2005.Sedimentary facies and subtlepetroleum reservoir of the Member2and lower Submember of Mem-ber1of Shahejie Formation of Paleogene on Lixian Slope of RaoyangSag,Central Hebei Province[J].Journal of Palaeogeography,7(3):373-381(in Chinese with English abstract).
Deng Yunhua.1999.Analysing the petroleum accumulational differenceof sag and uplift in Bohai Bay Basin[J].China Offshore Oil andGas(Geology),13(6):401-405(in Chinese with English ab-stract).
Hao Fang.2005.Kinetics of Hydrocarbon Generation and Mechanisms ofPetroleum Accumulation in Overpressured Basins[M].Beijing:Sci-ence Press,287-300(in Chinese).
Hou Guiting,Qian Xianglin,Song Xinmin.1998.The origin of the BohaiBay Basin[J].Acta Scientiarum Naturalium(Universitatis Pekinen-sis),34(4):503-509(in Chinese with English abstract).
Xu Changgui,Xu Xiaosong,Qiu Dongzhou,et al.2005.Structural andsequence stratigraphic frameworks and palaeogeography of the Paleo-gene in central-southern Liaoxi Sag,Liaodongwan Bay area[J].Journal of Palaeogeography,7(4):449-459(in Chinese with Eng-lish abstract).
Zhang Jinliang,Hou Yangshan,Lai Weiqing.1996.Reservoir character-istics of the Third Member of Shahejie Formation in NanmazhuangOilfield[J].Journal of Xi an Petroleum Institute,11(2):8-14(inChinese with English abstract).
Zhu Xiaomin,Xin Quanlin,Zhang Jinren.1994.Sedimentary characteris-tics and models of the beach-bar reservoirs in faulted down lacustrinebasins[J].Acta Sedimentologica Sinica,12(2):20-28(in Chi-nese with English abstract).
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