ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
黄骅坳陷中区古近系层序构成样式分析
  
关键词:Bohai Bay basin  Huanghua depression  sequence components  controlling factors
基金项目:中国地质大学(武汉)优秀青年教师资助计划项目(编号:CUGQNL0642); 湖北省杰出青年基金项目(编号:2003ABB012)
作者单位E-mail
廖远涛 中国地质大学资源学院湖北武汉430074 lyt706@163.com 
王振升 中国石油大港油田公司勘探开发研究院,天津大港300280  
肖敦清 中国石油大港油田公司勘探开发研究院,天津大港300280  
韦阿娟 中国石油大港油田公司勘探开发研究院,天津大港300280  
王家豪 中国地质大学资源学院湖北武汉430074  
严德天 中国科学院地质与地球物理研究所,北京100029  
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摘要:
Styles of Sequence Components in the Central Area of the Huanghua Depression
      Huanghua Depression is one of the most important oil and gas bearing basins in Bohai Bay basin of East China. On the basis of reflection characterisstics, well logging and other geological data, Shahejie Formation and Dongying Formation can be divided into three second-order sequences and eleven third-order sequences. Three system tracts can be recognized in each third-order sequence, which are lowstand system tract, expanding system tract and highstand system tract. Three typical tectonic backgrounds developed in the study area: ①Gentle slope characterized by slope break lies on the west side of Qinan sag, northwest side of Beidagang buried hill and its east-plunging part. Sequence styles of gentle slope break are developed in the above parts. ② Fault-controlled steep slope background can be seen on the south side of Nandagang buried hill and Beidagang buried hill. The above areas form the sequence style of fault-controlled steep slope. ③ The background of multilevel step-fault is Yangerzhuang fault terrace belt and the downthrow wall of Haihe fault. Tectonic activity is the main factor that controls the sequence components, and can be divided into microtectonic and local tectonic activities. Sediment source also mainly controls the sequence pattern.
LIAO Yuan-tao,WANG Zhen-sheng,XIAO Dun-qing,WEI A-juan,WANG Jia-hao,YAN De-tian.2008.Styles of Sequence Components in the Central Area of the Huanghua Depression[J].Acta Geoscientica Sinica,29(2):221-227.
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