南黄海海域生储盖层特征及油气远景评价
|
摘要
根据近年来新取得的资料,结合前人的研究成果,对南黄海海域的生储盖层特征进行了综合研究。古生界、中生界海相地层为南黄海海域的主力烃源岩,从构造运动和沉积发育情况分析,将南黄海海域的古生界、中生界海相地层生成油气的成藏过程划分为三叠纪印支运动前、侏罗纪-白垩纪、古近纪和新近纪4个阶段。通过对生储盖层的特征分析,说明南黄海古生界、中生界海相地层油气资源具有开发前景。在对南黄海盆地海相中生界、古生界烃源条件和后期保存条件研究的基础上,预测了盆地内海相油气资源的有利运聚区,为南黄海海域的油气勘探及研究工作提供了依据,对我国新的海上油气开发及部署作出了贡献。
According to new data and previous research results in recent years,the characteristics of reservoir and caprock of the South Yellow Sea were comprehensively investigated. Ancient marine Mesozoic strata were chosen as the main hydrocarbon source rocks. Based on the tectonic movement and sedimentary development analysis,the hydrocarbon accumulation in marine Mesozoic strata of South Yellow Sea is divided into four stages: stages before Triassic indosinian movement,Jurassic-Cretaceous,Paleogene and Neogene. This paper shows that ancient marine Mesozoic strata in the South Yellow Sea have the prospect of hydrocarbon development,through the analysis of the characteristics of the reservoir. The favorable marine oil and gas resources accumulation were forecasted based on the study of the hydrocarbon source and preservation condition in later period. This study provides the basis for oil and gas exploration and makes contribution to the deployment of new offshore oil and gas in China.
According to new data and previous research results in recent years,the characteristics of reservoir and caprock of the South Yellow Sea were comprehensively investigated. Ancient marine Mesozoic strata were chosen as the main hydrocarbon source rocks. Based on the tectonic movement and sedimentary development analysis,the hydrocarbon accumulation in marine Mesozoic strata of South Yellow Sea is divided into four stages: stages before Triassic indosinian movement,Jurassic-Cretaceous,Paleogene and Neogene. This paper shows that ancient marine Mesozoic strata in the South Yellow Sea have the prospect of hydrocarbon development,through the analysis of the characteristics of the reservoir. The favorable marine oil and gas resources accumulation were forecasted based on the study of the hydrocarbon source and preservation condition in later period. This study provides the basis for oil and gas exploration and makes contribution to the deployment of new offshore oil and gas in China.
引文
[1]汪龙文.南黄海的基本地质构造特征和油气远景[J].海洋地质与第四纪地质,1989,9(3):41-50.
[2]冯志强,姚永坚,曾祥辉,等.对黄海中、古生界地质构造及油气远景的新认识[J].中国海上油气(地质),2002,16(6):367-373.
[3]栾锡武.世界油气资源现状与未来发展方向[J].中国地质调查,2016,3(2):1-9.
[4]姚永坚,冯志强,郝天珧,等.对南黄海盆地构造层特征及含油气性的新认识[J].地学前缘,2008,15(6):232-240.
[5]蔡乾忠.黄海含油气盆地区域地质与大地构造环境[J].海洋地质动态,2002,18(11):8-12.
[6]程裕淇.中国区域地质概论[M].北京:地质出版社,1994:264.
[7]任纪舜.中国及邻区大地构造图(1∶5 000 000)[M].北京:地质出版社,1999:154.
[8]赵伟,韩文明,胡滨.东非裂谷Tanganyika地堑石油地质特征和勘探潜力分析[J].中国地质调查,2016,3(1):14-19.
[9]王金渝,周荔青,郭念发,等.苏浙皖石油天然气地质[M].北京:石油工业出版社,2000:139-144.
[10]张日华,信广林,刘希林,等.济阳拗陷滨海地区中生界油气研究与评价[J].山东国土资源,1994,10(1):32-39.
[11]赖万忠.黄海海域沉积盆地与油气[J].海洋地质动态,2002,18(11):13-16,2.
[12]戴春山,李刚.黄海海域前第三系及油气勘探[J].海洋地质动态,2002,18(11):21-22.
[13]翟光明.中国石油地质志[M].北京:石油工业出版社,1995:168-186.
[14]李刚,陈建文,肖国林,等.南黄海海域的海相中-古生界油气远景[J].海洋地质动态,2003,19(8):12-16,57-58.
[15]郭念发,俞凯.下扬子地区海相储集岩特征及含油气性[J].勘探家,1998,3(4):21-26.
[2]冯志强,姚永坚,曾祥辉,等.对黄海中、古生界地质构造及油气远景的新认识[J].中国海上油气(地质),2002,16(6):367-373.
[3]栾锡武.世界油气资源现状与未来发展方向[J].中国地质调查,2016,3(2):1-9.
[4]姚永坚,冯志强,郝天珧,等.对南黄海盆地构造层特征及含油气性的新认识[J].地学前缘,2008,15(6):232-240.
[5]蔡乾忠.黄海含油气盆地区域地质与大地构造环境[J].海洋地质动态,2002,18(11):8-12.
[6]程裕淇.中国区域地质概论[M].北京:地质出版社,1994:264.
[7]任纪舜.中国及邻区大地构造图(1∶5 000 000)[M].北京:地质出版社,1999:154.
[8]赵伟,韩文明,胡滨.东非裂谷Tanganyika地堑石油地质特征和勘探潜力分析[J].中国地质调查,2016,3(1):14-19.
[9]王金渝,周荔青,郭念发,等.苏浙皖石油天然气地质[M].北京:石油工业出版社,2000:139-144.
[10]张日华,信广林,刘希林,等.济阳拗陷滨海地区中生界油气研究与评价[J].山东国土资源,1994,10(1):32-39.
[11]赖万忠.黄海海域沉积盆地与油气[J].海洋地质动态,2002,18(11):13-16,2.
[12]戴春山,李刚.黄海海域前第三系及油气勘探[J].海洋地质动态,2002,18(11):21-22.
[13]翟光明.中国石油地质志[M].北京:石油工业出版社,1995:168-186.
[14]李刚,陈建文,肖国林,等.南黄海海域的海相中-古生界油气远景[J].海洋地质动态,2003,19(8):12-16,57-58.
[15]郭念发,俞凯.下扬子地区海相储集岩特征及含油气性[J].勘探家,1998,3(4):21-26.