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现代地质 ›› 2009, Vol. 23 ›› Issue (5): 865-871.

• 石油构造 • 上一篇    下一篇

古地貌恢复方法及应用——以济阳坳陷桩西地区沙二段为例

 姜正龙1, 邓宏文2, 林会喜3, 王林1   

  1. 1中国地质大学 海洋学院,北京100083;   2   中国地质大学 能源学院,北京100083;
    3中国石化 胜利油田分公司, 山东 东营257015
  • 收稿日期:2009-05-11 修回日期:2009-09-03 出版日期:2009-10-20 发布日期:2012-02-16
  • 作者简介:作者简介:姜正龙,男,副教授,1969年出生,矿产普查与勘探专业,主要从事盆地综合分析和评价的研究工作。Email:jiangzl@cugb.edu.cn。
  • 基金资助:

    中国石油科技创新基金项目(2008D-5006-01-09)

Methods and Application of Paleo-geomorphologies Rebuilding:An Example of the Second Member of Shahejie Formation, Zhuangxi Area, Jiyang Depression

 JIANG  Zheng-Long1, DENG  Hong-Wen2, LIN  Hui-Xi3, WANG  Lin1   

  1. 1School of Marine, China University of Geosciences, Beijing100083,China;
    2School of Energy Resources, China University of Geosciences, Beijing100083,China;
    3Shengli Oilfield Company,SINOPEC, Dongying,Shandong257015,China
  • Received:2009-05-11 Revised:2009-09-03 Online:2009-10-20 Published:2012-02-16

摘要:

济阳坳陷桩西地区沙二段埋深较大,应用残留厚度进行古地貌恢复存在较多问题。介绍了用压实法进行古地貌恢复的原理及方法。该方法分为视厚度校正、压实方程建立、单井压实厚度恢复、原始厚度图和古地貌图编制4个步骤。根据沙二段顶面构造图计算的真厚度校正系数最小可达0.83。压实结果表明压实率一般大于30%。结合视厚度校正、压实恢复结果和古水深,编制了沙二段基准面上升期和下降期的古地貌图,桩西地区沙二段古地貌中间高、东西两侧低。滩坝主要分布在孤北古隆起东西两侧,滩坝的发育明显受古隆起的控制。

关键词: 古地貌, 压实恢复, 滩坝, 视厚度校正, 沙二段, 济阳坳陷

Abstract:

This study applied the principle and methods of compaction restoration for reconstructing paleo-geomorphology of the Second Member of Shahejie Formation in Zhuangxi area of Jiyang Depression. The analyzing processes include four steps: (1) correcting of apparent thickness; (2) establishing of compaction equations;(3) restoring compaction of formations in each single drilling well; (4) composing maps of thickness of original layer and paleogeomorphology. As a result, the minimum value of correction coefficient for the real thickness was calculated as 0.83, based on structural map of the top of the Second Member of Shahejie Formation. The compaction rates are generally higher than 30%. Furthermore, the paleo-geomorphological maps of the Second Member of Shahejie Formation during uplift and subsidence sedimentary periods in Zhuangxi area were compiled. One highland in the middle and two sags in the eastern and the western sides of the Zhuangxi area were recognized from the maps. Beach bars occurred mainly along the two sides of Gubei paleo-uplift, suggesting the formation and development of beaches were clearly controlled by paleo-morphological uplift.

Key words: reconstruction of paleo-geomorphology, compaction restoration, beach bar, apparent thickness correcting, the Second Member of Shahejie Formation, Jiyang Depression

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