渤海湾盆地黄骅坳陷新生代沉降特征

董敏, 漆家福, 杨桥. 渤海湾盆地黄骅坳陷新生代沉降特征[J]. 地质科学, 2012, 47(3): 762-775.
引用本文: 董敏, 漆家福, 杨桥. 渤海湾盆地黄骅坳陷新生代沉降特征[J]. 地质科学, 2012, 47(3): 762-775.
Dong Min, Qi Jiafu, Yang Qiao. Tectonic subsidence characteristics ofHuanghua depression in Bohai Bay Basin in Cenozoic[J]. Chinese Journal of Geology, 2012, 47(3): 762-775.
Citation: Dong Min, Qi Jiafu, Yang Qiao. Tectonic subsidence characteristics ofHuanghua depression in Bohai Bay Basin in Cenozoic[J]. Chinese Journal of Geology, 2012, 47(3): 762-775.

渤海湾盆地黄骅坳陷新生代沉降特征

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    通讯作者: 漆家福, 男, 1957年8月生,博士,教授,构造地质学和石油地质学学专业。E-mail: qijiafu@cup.edu.cn
  • 中图分类号: P542

Tectonic subsidence characteristics ofHuanghua depression in Bohai Bay Basin in Cenozoic

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    Corresponding author: Qi Jiafu
  • 在对渤海湾盆地黄骅坳陷区域构造特征的22条地震剖面解释的基础上,分析了黄骅坳陷沉降特征。通过对黄骅坳陷的9个主要凹陷沉降史的研究表明,黄骅坳陷新生代构造沉降量的时空差异性分布明显。时间上,黄骅坳陷具有"幕式"沉降特征,孔店组沉积期为裂陷Ⅰ幕、沙三段沉积期为裂陷Ⅱ幕、沙一段和沙二段沉积期和东营组沉积期为裂陷Ⅲ幕、馆陶组和明化镇组下段沉积期为热沉降幕、明化镇组上段和第四系的沉积期为加速热沉降幕。不同沉积期盆地沉降在空间分布上,沉降速率上都有明显差异。通过对凹陷尺度单井的埋藏史曲线,构造沉降曲线,基底沉降图和沉降中心迁移图对比分析表明,空间上,黄骅坳陷新生代沉降作用具有明显的迁移规律,总体是自南向北,自西向东迁移,现今的沉降中心位于歧口凹陷海域部分。
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出版历程
收稿日期:  2012-04-06
修回日期:  2012-05-23
刊出日期:  2012-07-25

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