珠江口盆地番禺低隆起韩江组下段层序地层与有利目标预测
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摘要
综合利用钻井、测井、地震资料,运用层序地层学原理,在珠江口盆地番禺低隆起韩江组下段识别出4个层序界面,划分为3个3级层序,即SQ1、SQ2、SQ3。通过井-震划分对比,建立了工区内韩江组下段层序地层等时格架。在等时格架建立的基础上,总结出研究区发育的3种岩性地层圈闭,主要受层序界面、最大海泛面、初始海泛面控制。
By comprehensively using well drilling,logging and seismic data and sequence stratigraphic principles,the lower segment of Hanjiang Formation of Panyu low uplift in Pearl-river Mouth Basin was recognized as 4 sequence boundaries and it was divided into 3 third-order sequences,including SQ1,SQ2 and SQ3.According to well-seismic division and comparison,isochronal sequence stratigraphic framework of lower segment of Hanjiang formation was established.On the basis of the isochronal sequence stratigraphic framework,three kinds of litho-stratigraphic traps were summed up in the studied area,they were mainly controlled by sequence boundary,maximum flooding surface and initial flooding surface.
引文
[1]陈长民,施和生,许仕策.珠江口盆地(东部)第三系油气藏形成条件[M].北京:科学出版社,2003.
    [2]朱筱敏.层序地层学[M].东营:石油大学出版社,2000.
    [3]威尔格斯.层序地层学原理(海平面变化综合分析)[M].徐怀大,魏魁生,洪卫东,译.北京:石油工业出版社,1993.
    [4]贺子倩,张尚锋,淡卫东,等.准噶尔盆地红车断裂带侏罗系层序地层特征[J].石油天然气学报,2008,30(1):202~205.
    [5]贾承造,赵文智,邹才能,等.岩性油气藏勘探研究的两项核心技术[J].石油勘探与开发,2004,31(3):8~9.
    [6]Vail P R.Seismic stratigraphyinterpretation using sequence stratigraphy.Part 1:seismic stratigraphyinterpretation procedure[A].Bally A W.Atlas of seismic stratigraphy[C].AAPG Studies in Geology,1987.

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