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南堡凹陷馆陶组火山事件及其油气地质意义

VOLCANIC EVENTS AT THE STAGE OF GUANTAO FORMATION IN NANPU SAG AND ITS PETROLEUM GEOLOGICAL SIGNIFICANCE

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【作者】 林正良王华姜华赵淑娥徐德英康海涛曹中宏

【Author】 LIN Zhengliang1,2,WANG Hua1,JIANG Hua3,ZHAO Shue1, XU Deying4,KANG Haitao4,CAO Zhonghong4(1 Key Laboratory of Tectonics and Petroleum Resources,China University of Geosciences,Wuhan 430074; 2 Key Laboratory of Biogeology and Environmental Geology of Ministry of Education,China University of Geosciences, Wuhan 430074;3 PetroChina Institute of Petroleum Exploration& Development,Beijing 100083; 4 PetroChina Jidong Oilfield Company,Tangshan 063004)

【机构】 中国地质大学构造与油气资源教育部重点实验室中国地质大学生物地质与环境地质教育部重点实验室中国石油勘探开发研究院石油地质所中国石油冀东油田公司

【摘要】 南堡凹陷新近系馆陶组地层沉积时期凹陷内火山活动剧烈。通过测井分析及地震解释表明,火山喷发物的岩性以玄武岩为主,形成于新近系早期。平面分布上具有东北薄、西南厚,纵向上具有多期叠置发育的特点。综合分析认为,大量的火山物质改变了凹陷的地貌形态,影响了后继河流相沉积地层的空间分布,在西部地区形成大量的地层圈闭。由于火山事件的热作用,改变了凹陷内的地温场分布,导致烃源岩的异常热演化,对凹陷内油气生成具有重要促进作用。火山岩体的封隔作用可以形成多种类型的圈闭,对后期油气的运移、聚集及分布等方面具有重要的影响。

【Abstract】 The volcanic eruption was intensive and frequent in the Nanpu Sag during the period of Neogene when the Guantao Formation was deposited.Through logging and seismic interpretation,it is revealed that the volcanic rocks were mainly basalt in lithology formed in the early Neogene.The volcanic sequence is thicker in the southwest and thinner in the northeast,and formed by multi-stage eruption.The comprehensive study suggests that the eruption of huge amount of volcanic materials changed the geomorphology of the Sag,that influenced the spatial distribution of the fluvial strata deposited later on.Many stratigraphic traps were formed in the west of the Sag.The volcanic activities also brought changes in the geothermal field in the Sag,which led to the abnormal evolution of source rocks,and greatly accelerated the hydrocarbon generation process within the Sag.Acting as an effective sealing,volcanic bodies could be the cover of many types of traps.The significance of the volcanic rocks should never be underestimated in hydrocarbon migration,accumulation,and distribution.

【基金】 国家自然科学基金项目(40872077);构造与油气资源教育部重点实验室基金项目(TPR-2010-08);湖北省自然科学基金重点项目(2008CDA098)
  • 【文献出处】 海洋地质与第四纪地质 ,Marine Geology & Quaternary Geology , 编辑部邮箱 ,2011年03期
  • 【分类号】P618.13
  • 【被引频次】4
  • 【下载频次】252
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