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方正断陷方4井区白垩—古近系层序界面识别标志
Identification of Sequence Stratigraphy in Fang4 Well Area in Cretaceous and Paleogene,Fangzheng Fault Depression
【摘要】 本文应用沉积学原理,层序地层学等原理和方法,依据测井,录井等资料,进行了各级层序单元的识别与划分,建立了方4井白垩-古近系各层序界面的识别标志,井震结合,进行层序地层划分对比,将白垩-古近系划分为十个三级层序,并总结了各层序地层单元特征。
【Abstract】 By using theory of sedimentology and sequence stratigraphy,Based on logging and logging data,established high precision sequence formation frame.We established identification sign of every sequence interface of Cretaceous and Paleogene on the basis of sequence stratigraphy,at the same time we made dividing and comparing for the sequence formation combining well data and seismic data and certification each other.We divided Cretaceous and Paleogene into ten tertiary sequences,then concluded unit feature of every sequence formation.
【关键词】 方正断陷;
层序界面;
测井相;
地震相;
【Key words】 Fangzheng Fault; Sequence Boundary; Log Facies; Seismic Facies;
【Key words】 Fangzheng Fault; Sequence Boundary; Log Facies; Seismic Facies;
- 【文献出处】 内蒙古石油化工 ,Inner Mongolia Petrochemical Industry , 编辑部邮箱 ,2010年01期
- 【分类号】P539.2
- 【被引频次】2
- 【下载频次】105