济阳坳陷沾化凹陷沙一下亚段优质烃源岩成因分析
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摘要
沾化凹陷发育沙四上亚段、沙三下亚段和沙一下亚段3套烃源岩,前人对沙一下亚段烃源岩未进行深入研究。本文利用有机地球化学方法对沾化凹陷沙一下亚段烃源岩品质进行分析,研究表明沙一下亚段烃源岩有机质丰度高、干酪根类型以Ⅰ型为主,为优质烃源岩;烃源岩沉积中心位于渤南洼陷,但孤南洼陷烃源岩品质最好。孤北洼陷和孤南洼陷的部分烃源岩达到大量排烃阶段,所以勘探开发研究应重视来自沙一下亚段烃源岩的贡献。沉积环境分析表明,沙一下亚段沉积期沾化凹陷构造沉降速率较小,气候为北亚热带至暖温带中等偏干旱气候,均不支持形成优质烃源岩。沙一下亚段高品质烃源岩的形成的主要原因是高盐度导致湖泊的高生产力和良好的水体分层。湖盆高盐度是由于鲁佩期的海侵导致,海侵沿孤南洼陷—孤北洼陷—渤南洼陷的方向推进,导致孤南洼陷虽然不是沉积、沉降中心,但烃源岩品质最好。
Objectives: The Zhanhua Sag developed three sets of source rocks,which include the upper Es4( the 4 th Member of the Eocene Shahejie Formation),the lower Es3 and the lower Es1( i.e. the 4 th,3 rd and 1 st Member of the Eocene Shahejie Formation). There have been a few studies on source rocks of the lower Es1 before.Methods: Analyzed source rocks qualities of the lower Es1 in the Zhanhua Sag by using organic geochemical methods.Results: the result shows that source rocks of the lower Es1 had high abundance of organic matter,which kerogen are mainly typeⅠ,are high-quality hydrocarbon source rocks. Source rocks deposited center is located in the Bonan Subsag,but best quality source rocks situated in the Gunan Subsag. Part of the hydrocarbon source rocks are in mature stage in the Gubei Subsag and the Gunan Subsag,so exploration and development research should pay attention to contribution of the lower Es1 hydrocarbon source rocks. Depositional environments analysis showed that tectonic subsidence rate was smaller and the climate was the north subtropical to warm temperate middle arid climate during sedimentary period of the lower Es1 in the Zhanhua Sag,didn't support the formation of high-quality hydrocarbon source rocks. High productivity and good water column caused by high salinity was the main reason of the formation of high-quality hydrocarbon source rocks in the lower Es1. High salinity was due to marine transgression in Lupen.Conclusions: Marine transgressived along the direction of the Gunan Subsag—Gubei Subsag—Bonan Subsag,caused the Gunan Subsag had best quality source rocks though it was not sedimentary center and sedimentation center.
Objectives: The Zhanhua Sag developed three sets of source rocks,which include the upper Es4( the 4 th Member of the Eocene Shahejie Formation),the lower Es3 and the lower Es1( i.e. the 4 th,3 rd and 1 st Member of the Eocene Shahejie Formation). There have been a few studies on source rocks of the lower Es1 before.Methods: Analyzed source rocks qualities of the lower Es1 in the Zhanhua Sag by using organic geochemical methods.Results: the result shows that source rocks of the lower Es1 had high abundance of organic matter,which kerogen are mainly typeⅠ,are high-quality hydrocarbon source rocks. Source rocks deposited center is located in the Bonan Subsag,but best quality source rocks situated in the Gunan Subsag. Part of the hydrocarbon source rocks are in mature stage in the Gubei Subsag and the Gunan Subsag,so exploration and development research should pay attention to contribution of the lower Es1 hydrocarbon source rocks. Depositional environments analysis showed that tectonic subsidence rate was smaller and the climate was the north subtropical to warm temperate middle arid climate during sedimentary period of the lower Es1 in the Zhanhua Sag,didn't support the formation of high-quality hydrocarbon source rocks. High productivity and good water column caused by high salinity was the main reason of the formation of high-quality hydrocarbon source rocks in the lower Es1. High salinity was due to marine transgression in Lupen.Conclusions: Marine transgressived along the direction of the Gunan Subsag—Gubei Subsag—Bonan Subsag,caused the Gunan Subsag had best quality source rocks though it was not sedimentary center and sedimentation center.
引文
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刘培,蒋有录,刘华,熊伟,李克成,朱荣伟.2013.渤海湾盆地沾化凹陷断层活动与新近系油气成藏关系.天然气地球科学,24(3):541～547.
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