车镇凹陷层序地层与石油地质研究
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摘要
车镇凹陷为渤海湾盆地济阳坳陷北部的一个次级凹陷。在综合分析地震、测
井、岩芯、录井、古生物等资料的础上,将车镇凹陷下第三系沙三段一东营组沉
积共划分出2个二级层序、6个三级层序。在此基础之上,探讨了控制层序发育
的地质因素和沉积层序的形成机制,将研究区的层序地层模式划分为陡坡带模式、
缓坡带模式和洼陷带模式三种类型。对沉积体系进行了详细研究,认为车镇凹陷
古近系发育8种沉积相类型,对其时空演化规律和平面分布特征进行了分析。在
对研究区烃源岩地质及地球化学特征研究的基础上,进行了油源对比分析,认为
围绕义和庄凸起的郭局子洼陷、大王北洼陷、车西洼陷和四扣洼陷都不同程度地
向义和庄凸起及其北坡提供了油气,义和庄凸起潜山带油气主要来自四扣沣陷沙
三段烃源岩,郭局子地区油气来自北部的郭局子洼陷沙三段烃源岩,大王庄鼻状
构造带油气来自大王北洼陷沙三、沙一段烃源岩。在分析了研究区油气藏类型的
基础上,探讨了各时期油气藏的成藏机理,并着重研究了车镇凹陷岩性油气藏的
成藏机理。最后,分析了层序、沉积体系与油气分布之间的关系。
Chezhen sag, a sub-depression of the Jiyang depression, is located at the north of the Jiyang depression, which belongs to the Bohaiwan basin. Based on the materials of seismic exploration, well-logging, drilling core and paleontology etc., the Es3-Ed of the Chezhen sag has been divided into 2 2nd-order sequences and 6 3rd-order sequences. And on this base, the geological factors which control the development of the sequences and the formation mechanism of sedimentary sequences have been discussed. The sequence models include 3 types, they are escarpment pattern, flat ramp pattern and depression pattern. The sedimentary system has been studied in detail. It has been considered that the Chezhen sag has developed 8 kinds of facies. The evaluation rules and distribution features have been analyzed. Based on the study of the geological and geochemical characters of the source rock, the source comparison considered that the oil in the Yihezhuang relief and its north part is partly from Guojuzi sag, Dawangbei sag, Chexi sag and Sikou sag. Oil in the Yihezhuang buried hill comes from Es3 source in the Sikou sag mainly. The oil in the Guojuzi area comes from Es3 source in the Guojuzi sag. The oil in Dawangzhang mainly comes from the Es3 and Es1 source in the Dawangbei sag. Based on the analysis of the reservoir types, the formation mechanism of the reservoir in different period has been discussed. And the lithological reservoir has been studied as a important part. At last, the relationship among the sequence, sedimentary system and oil distribution has been analyzed.
井、岩芯、录井、古生物等资料的础上,将车镇凹陷下第三系沙三段一东营组沉
积共划分出2个二级层序、6个三级层序。在此基础之上,探讨了控制层序发育
的地质因素和沉积层序的形成机制,将研究区的层序地层模式划分为陡坡带模式、
缓坡带模式和洼陷带模式三种类型。对沉积体系进行了详细研究,认为车镇凹陷
古近系发育8种沉积相类型,对其时空演化规律和平面分布特征进行了分析。在
对研究区烃源岩地质及地球化学特征研究的基础上,进行了油源对比分析,认为
围绕义和庄凸起的郭局子洼陷、大王北洼陷、车西洼陷和四扣洼陷都不同程度地
向义和庄凸起及其北坡提供了油气,义和庄凸起潜山带油气主要来自四扣沣陷沙
三段烃源岩,郭局子地区油气来自北部的郭局子洼陷沙三段烃源岩,大王庄鼻状
构造带油气来自大王北洼陷沙三、沙一段烃源岩。在分析了研究区油气藏类型的
基础上,探讨了各时期油气藏的成藏机理,并着重研究了车镇凹陷岩性油气藏的
成藏机理。最后,分析了层序、沉积体系与油气分布之间的关系。
Chezhen sag, a sub-depression of the Jiyang depression, is located at the north of the Jiyang depression, which belongs to the Bohaiwan basin. Based on the materials of seismic exploration, well-logging, drilling core and paleontology etc., the Es3-Ed of the Chezhen sag has been divided into 2 2nd-order sequences and 6 3rd-order sequences. And on this base, the geological factors which control the development of the sequences and the formation mechanism of sedimentary sequences have been discussed. The sequence models include 3 types, they are escarpment pattern, flat ramp pattern and depression pattern. The sedimentary system has been studied in detail. It has been considered that the Chezhen sag has developed 8 kinds of facies. The evaluation rules and distribution features have been analyzed. Based on the study of the geological and geochemical characters of the source rock, the source comparison considered that the oil in the Yihezhuang relief and its north part is partly from Guojuzi sag, Dawangbei sag, Chexi sag and Sikou sag. Oil in the Yihezhuang buried hill comes from Es3 source in the Sikou sag mainly. The oil in the Guojuzi area comes from Es3 source in the Guojuzi sag. The oil in Dawangzhang mainly comes from the Es3 and Es1 source in the Dawangbei sag. Based on the analysis of the reservoir types, the formation mechanism of the reservoir in different period has been discussed. And the lithological reservoir has been studied as a important part. At last, the relationship among the sequence, sedimentary system and oil distribution has been analyzed.
引文
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