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莱州湾凹陷烃源岩生烃历史模拟
引用本文:姜丽娜.莱州湾凹陷烃源岩生烃历史模拟[J].科技导报(北京),2011,29(13):52-56.
作者姓名:姜丽娜
作者单位:1. 中国石油天然气股份有限公司大庆油田勘探开发研究院,黑龙江大庆 163712;2. 中国石油大学(北京);油气资源与探测国家重点实验室,北京 102249
基金项目:国家自然科学基金重点项目(90914006)
摘    要: 本文通过运用IES盆地模拟的方法,采用Easy%Ro模型,以单井的热史和生烃史为基础,从剖面和平面两方面研究了莱州湾凹陷两套主力烃源岩沙三段和沙四段在不同时期不同区域生烃状态。研究表明,在明化镇组下段沉积末期(5.1Ma)北洼沙三段烃源岩已广泛进入生烃门限,沙四段烃源岩大范围生排烃;现今北洼沙三段烃源岩大量排烃,沙四段烃源岩排烃范围进一步扩大,北洼中心处已进入生烃高峰。

关 键 词:莱州湾凹陷    烃源岩    盆地模拟    生烃历史

Simulation of Hydrocarbon Generation History of Source Rocks in Laizhouwan Sag
JIANG Lina, .Exploration , Development Research Institute,Daqing Oilfield Company,China National Petroleum Corporation,Daqing ,Helongjiang Province,China .State Key Laboratory of Petroleum Resource , Prospecting,China University of Petroleum,Beijing ,China.Simulation of Hydrocarbon Generation History of Source Rocks in Laizhouwan Sag[J].Science & Technology Review,2011,29(13):52-56.
Authors:JIANG Lina  Exploration  Development Research Institute  Daqing Oilfield Company  China National Petroleum Corporation  Daqing  Helongjiang Province  China State Key Laboratory of Petroleum Resource  Prospecting  China University of Petroleum  Beijing  China
Institution:1. Exploration and Development Research Institute, Daqing Oilfield Company, China National Petroleum Corporation, Daqing 163712, Helongjiang Province, China;2. State Key Laboratory of Petroleum Resource and Prospecting; China University of Petroleum, Beijing 102249, China
Abstract:In this paper,the IES basin modeling method and the model of Easy%Ro are firstly used to analyze the single well thermal history and the hydrocarbon generation history.The third member of Shahejie Formation(Es3) and the fourth member of Shahejie Formation(Es4) are the major source rocks in Laizhouwan Sag.Based on the study of the single well thermal history and the hydrocarbon generation history,the hydrocarbon states of the two major source rocks in different periods and different areas are discussed.It is...
Keywords:Laizhouwan Sag  source rocks  basin modeling  hydrocarbon generation history  
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