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北黄海东部次盆地中新生代原型盆地分析
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  • 英文篇名:Analysis of Meso-Cenozoic prototype basins in the East sub-basin,northern Yellow Sea
  • 作者:简晓玲 ; 刘金萍 ; 王改云
  • 英文作者:JIAN Xiaoling;LIU Jinping;WANG Gaiyun;MLR Key Laboratory of Marine Mineral Resources;Guangzhou Marine Geological Survey;
  • 关键词:北黄海 ; 东部次盆地 ; 原型盆地 ; 中新生代 ; 构造演化
  • 英文关键词:northern Yellow Sea;;East sub-basin;;prototype basin;;Meso-Cenozoic;;tectonic evolution
  • 中文刊名:ZHSD
  • 英文刊名:China Offshore Oil and Gas
  • 机构:国土资源部海底矿产资源重点实验室;广州海洋地质调查局;
  • 出版日期:2019-02-20
  • 出版单位:中国海上油气
  • 年:2019
  • 期:v.31
  • 基金:中国地质调查局项目(编号:DD20189828)部分研究成果
  • 语种:中文;
  • 页:ZHSD201901003
  • 页数:10
  • CN:01
  • ISSN:11-5339/TE
  • 分类号:26-35
摘要
北黄海东部次盆地勘探程度较低,是中新生代小型叠合断陷盆地,经历了多期构造运动,盆地构造复杂。利用最新的地震和钻井资料,从构造特征分析入手,结合盆地发育的动力学背景,梳理了北黄海东部次盆地的构造演化,认为该盆地中新生代发育了伸展裂陷盆地、走滑伸展盆地及坳陷盆地3类性质的原型盆地。中—晚侏罗世,表现单一的断裂走向和箕状断陷型结构,为伸展裂陷型盆地,是该时期区域左旋剪切应力在盆地内派生的NE—SW向拉张应力作用的结果;早白垩世—晚渐新世,经历了早期区域左旋剪切应力向晚期区域右旋剪切应力的转变,表现为箕状断陷结构兼具明显走滑张扭特征,为走滑伸展盆地;中新世—第四纪,为典型的裂后沉降型坳陷盆地。盆地发育演化过程主体表现为由新生代受F2断裂控制的NEE向断陷盆地叠加在中生代受F1断裂控制的NW向断陷盆地之上,之后进入裂后坳陷沉降阶段;沉积沉降中心经历了先NW向迁移再NEE向迁移的过程。
        The East sub-basin in northern Yellow Sea is a small-scale Meso-Cenozoic superimposed faulted basin with a low degree of exploration.The basin has undergone multi-stage tectonic movements,and exhibits complex tectonic conditions.Combining the structural feature with dynamic settings of basin development,and by utilizing the latest seismic and drilling data,this paper studied the tectonic evolution process of the East sub-basin in northern Yellow Sea,and concluded that three types of prototype basins,namely extensional rifting basin,strike-slip extension basin and depression basin were developed in this basin during Meso-Cenozoic period.During the middlelate Jurassic,an extensional rifting basin,appearing as the single fault orientation and the dustpan-shaped rift structure,was developed due to the NE—SW tensile stress induced by the left-lateral shear stress in this period.During the early Cretaceous—late Oligocene,a strike-slip extension basin was developed.It experienced the transition from the left-lateral shear stress in the early region to the right-lateral shear stress in the late region,characterized by dustpan-shaped rift structure and obvious strike-slip tenso-shear feature.During the Miocene—Quaternary,a typical post-rift subsidence depression basin was developed.The features of evolution process of basin development are:the NEE rift basin controlled by the F2 fault in the Cenozoic is superimposed on the NW rift basin controlled by the F1 fault in the Mesozoic;then it experienced a post-rift depression subsidence stage;the subsidence center migrated from NW to NEE.
引文
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