惠民凹陷火山活动的成烃热效应
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摘要
长期以来油气地质研究与勘探重点集中在碎屑岩油气藏,火成岩油气藏的形成和分布理论研究相对滞后,火成岩对烃源岩的热作用方面的研究更是少之又少。随着隐蔽油气藏越来越受到重视,火成岩油气藏作为一种重要的隐蔽油气藏类型,其地位显得日益重要,研究火山活动带来的热量对成烃方面的影响,对有效地指导勘探实践有重要的意义。
惠民凹陷以及邻区古近纪和新近纪岩浆活动划可分为4个亚期与两大期:即孔店期、沙四段沉积时期、沙三段沉积时期、东营期、馆陶期,其中前四期构成了古近纪火山活动旋回,第五期构成新近纪火山活动旋回。惠民凹陷火成岩主要发育在阳信洼陷的东部和中央隆起带附近。通过对惠民凹陷的火成岩油气藏的原油的地球化学特征,发现研究区为淡水湖相的还原环境,大部分的样品是低熟油,有一小部分是成熟油。阳信洼陷的火成岩区与非火成岩区的烃源岩的对比、夏38井的烃源岩在纵向上和横向上的对比、火成岩油气藏原油与常规原油的对比,发现火成岩引起了地温场的改变,对烃源岩提供了热量,使得烃源岩受的烘烤,成熟度变大,埋藏较浅的烃源岩提前进入生烃门限,并且距离侵入体越近,作用越明显。带来的热量对原油的成熟度同样也产生了类似的影响,在同一地区,同一层位,同一源岩,同一期次火山活动的条件下,火成岩油气藏原油比常规原油的热演化程度要高,在此基础上建立了火成岩促使烃源岩热成熟的模式。
The research and exploration of petroleum geology has emphatically focused on clastic reservoir for a long time, which leads to the theoretical study of igneous reservoir's formation and distribution later than exploration practice. However, the research of igneous rock having thermal effect on Source Rock is much less. With the subtle reservoir being more and more important, igneous reservoir has been one kind of subtle reservoirs.and it's position is increasingly important, especially the research of heat quantity with volcanic activity having effect on hydrocarbon generation is meaningful for effectively guiding oil and gas exploration.
Magmatism in Huimin sag and its adjacent area is divided into four sub stages and two stages, that is Kongdian formation, Sha-4 member, Sha-3 member, Dongying formation, and Guantao formation, with the first four stages made up one magmatism cycle in Paleogene and the last the cycle in Neogene .Igneous rocks in Huimin sag mainly developed at the east of Yangxin subsag and near the central uplift belt. Oil biomarkers of igneous reservoirs in Huimin sag is analysised, which suggested that the research area is lacustrine reduction environment, with higher plants be the main oil source. Most samples are immature oil, and few are mature.Through the comparisons of Source Rock between igneous province and non-igneous province in Yangxin sub-depression, Source Rock of Xia-38 well at lateral and vertical and maturity of crude oil in reservoir between igneous reservoir and clastic reservoir, these comparisons found that igneous rock changed geothermal field, provided heat to Source Rock, baked Source Rock, and made Source Rock mature. Source Rock buried shallow can earlier enter oil generation threshold. This effect is more obvious within the nearer limit of intrusive igneous rock. These comparisons also found that it becomes similar effect to crude oil in reservoir, in other words, under the same area, same stratigraphic horizon, similar Source Rock and identical volcanic activity circumstances, the crude oil in igneous reservoir had higher thermal evolution degree than normal crude oil. This paper finally established the models of igneous rock impelling Source Rock mature.
惠民凹陷以及邻区古近纪和新近纪岩浆活动划可分为4个亚期与两大期:即孔店期、沙四段沉积时期、沙三段沉积时期、东营期、馆陶期,其中前四期构成了古近纪火山活动旋回,第五期构成新近纪火山活动旋回。惠民凹陷火成岩主要发育在阳信洼陷的东部和中央隆起带附近。通过对惠民凹陷的火成岩油气藏的原油的地球化学特征,发现研究区为淡水湖相的还原环境,大部分的样品是低熟油,有一小部分是成熟油。阳信洼陷的火成岩区与非火成岩区的烃源岩的对比、夏38井的烃源岩在纵向上和横向上的对比、火成岩油气藏原油与常规原油的对比,发现火成岩引起了地温场的改变,对烃源岩提供了热量,使得烃源岩受的烘烤,成熟度变大,埋藏较浅的烃源岩提前进入生烃门限,并且距离侵入体越近,作用越明显。带来的热量对原油的成熟度同样也产生了类似的影响,在同一地区,同一层位,同一源岩,同一期次火山活动的条件下,火成岩油气藏原油比常规原油的热演化程度要高,在此基础上建立了火成岩促使烃源岩热成熟的模式。
The research and exploration of petroleum geology has emphatically focused on clastic reservoir for a long time, which leads to the theoretical study of igneous reservoir's formation and distribution later than exploration practice. However, the research of igneous rock having thermal effect on Source Rock is much less. With the subtle reservoir being more and more important, igneous reservoir has been one kind of subtle reservoirs.and it's position is increasingly important, especially the research of heat quantity with volcanic activity having effect on hydrocarbon generation is meaningful for effectively guiding oil and gas exploration.
Magmatism in Huimin sag and its adjacent area is divided into four sub stages and two stages, that is Kongdian formation, Sha-4 member, Sha-3 member, Dongying formation, and Guantao formation, with the first four stages made up one magmatism cycle in Paleogene and the last the cycle in Neogene .Igneous rocks in Huimin sag mainly developed at the east of Yangxin subsag and near the central uplift belt. Oil biomarkers of igneous reservoirs in Huimin sag is analysised, which suggested that the research area is lacustrine reduction environment, with higher plants be the main oil source. Most samples are immature oil, and few are mature.Through the comparisons of Source Rock between igneous province and non-igneous province in Yangxin sub-depression, Source Rock of Xia-38 well at lateral and vertical and maturity of crude oil in reservoir between igneous reservoir and clastic reservoir, these comparisons found that igneous rock changed geothermal field, provided heat to Source Rock, baked Source Rock, and made Source Rock mature. Source Rock buried shallow can earlier enter oil generation threshold. This effect is more obvious within the nearer limit of intrusive igneous rock. These comparisons also found that it becomes similar effect to crude oil in reservoir, in other words, under the same area, same stratigraphic horizon, similar Source Rock and identical volcanic activity circumstances, the crude oil in igneous reservoir had higher thermal evolution degree than normal crude oil. This paper finally established the models of igneous rock impelling Source Rock mature.
引文
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