饶阳凹陷大王庄地区古近系层序地层特征
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
运用地层基准面原理和分析方法,综合研究钻井、测井和三维地震资料,在饶阳凹陷大王庄地区古近系识别出两种层序界面类型———不整合面和沉积作用转换面;在井-震精细标定的基础上建立了层序地层格架。饶阳凹陷大王庄地区古近系东营组至沙三段发育9个层序界面,将其划分为2个超长期基准面旋回(二级层序)和8个长期基准面旋回(三级层序);分析古近系不同层序基准面上升期与下降期地层叠加样式及沉积相、沉积微相构成。确定沙一段是大王庄地区最重要的岩性油藏勘探目的层系,其储集层类型主要为三角洲前缘分流河道砂和滩坝砂;有利储集相带主要分布于基准面上升期和下降期的早期。
The identification signs of the Paleogene sequence boundary are distinguished and two kinds of sequence boundaries,unconformity and shift surface of deposition,are identified according to drilling,logging and 3D seismic data in Dawangzhuang area,Raoyang sag by using the ways and principles of the high resolution sequence stratigraphy.Two super-term stratigraphic base level circles(the 2nd sequence) and the corresponding 8 long-term stratigraphic base level circles(the 3rd sequence) could be distinguished in Paleogene in the study area within the nine sequence boundaries.Stratigraphic frames are built on the basis of the well and seismic-data calibration.It is confirmed that the first segment of Shahejie Formation is the key target series for exploration in the study area according to the sedimentary facies,Which reservoir sands are the beach bar and distributary channel sandstone of delta front.The distribution of advantaged reservoir is closely related to their position in the sequence and mainly developed at the half cycle of increasing and the early of the descending base level cycle.
引文
操应长,姜在兴,夏斌,等.2003.利用测井资料识别层序地层界面的几种方法[J].石油大学学报(自然科学版),27(2):23-26.
    崔周旗,李文厚,李莉,等.2005.冀中饶阳凹陷蠡县斜坡古近系沙河街组沙二段及沙一段下亚段沉积相与隐蔽油藏[J].古地理学报,7(3):373-381.
    邓宏文,C ross T A,王洪亮,等.2002.高分辨率层序地层学———原理及应用[M].北京:地质出版社,1-46.
    侯凤香,王海潮,宫玉,等.2005.饶阳凹陷蠡县斜坡综合地质研究及目标评价[M]//华北油田公司勘探开发研究院《古潜山》编辑部,华北油田勘探开发科技文选(2003年).北京:石油工业出版社,73-80.
    唐智,吴华元等.1988.中国石油地质志(5)-华北油田[M].北京:石油工业出版社,94-95.
    张文朝,崔周旗,韩春元,等.2001.冀中坳陷老第三纪湖盆演化与油气[J].古地理学报,3(1):45-54.
    张振生,黎英,王冰.1997.冀中坳陷陆相地层层序地层学的应用[J].石油学报,18(2):26-34.

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心