方正断陷方4井区白垩—古近系层序界面识别标志

详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文

英文篇名：Identification of Sequence Stratigraphy in Fang4 Well Area in Cretaceous and Paleogene,Fangzheng Fault Depression 中文刊名：内蒙古石油化工 英文刊名：Inner Mongolia Petrochemical Industry 作者：聂志阳 ; 王桂芳 英文作者：NIE Zhi-yang1 ; WANG Gui-fang2(1.Exploration and Development Research Institute of PetroChina Daqing Oilfield Co. ; Ltd ; Daqing ; Heilongjiang ; 163712 ; China ; 2.College of Geosciences ; Daqing Petroleum Institute ; Daqing ; Heilongjiang ; 163318 ; China) 中文关键词：方正断陷 ; 层序界面 ; 测井相 ; 地震相 英文关键词：Fangzheng Fault ; Sequence Boundary ; Log Facies ; Seismic Facies 出版日期：2010-01-15 机构：大庆油田有限责任公司勘探开发研究院;大庆石油学院地球科学学院; 年：2010 期：01 出版单位：内蒙古石油化工

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。
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.

引文

[1]郑荣才,尹世民,彭军.基准面旋回结构与叠加样式的沉积动力学分析[J].沉积学报,2000,18(3):369~375.
    [2]Vail P.R.Sequence stratigraphy workbook,fundamentals of sequence stratigraphy[J].AAPG Annual Convention Short Course:Sequence Stratigraphy Interpretation ofSeismic Well and Outcrop Data,presentedby P.R.Vail and J.B.Sangree,March 19,1988,Houston,Texas.
    [3]赵澄林,朱筱敏.沉积岩石学[J].北京工业出版社,2001.
    [4]李新虎,测井曲线最优特征值在层序界面识别中的应用[J].湖南科技大学学报,2006,21(3):26.
    [5]纪友亮,层序地层学[M].同济大学出版社,2005.