ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
鄂尔多斯盆地西峰油田三叠系延长组浊流沉积及成因模式
  
关键词:Ordos Basin  Yanchang Formation  turbidity current deposit  genetic model
基金项目:中国科学院知识创新工程重要方向项目(编号:KZCX3-SW-128); 国家自然科学基金项目(编号:40272065)
作者单位E-mail
卢龙飞 同济大学海洋与地球科学学院海洋地质国家重点实验室上海200092中国科学院兰州地质研究所兰州730000 llf779712@yahoo.com.cn 
史基安 中国科学院兰州地质研究所兰州730000  
蔡进功 同济大学海洋与地球科学学院海洋地质国家重点实验室上海200092  
王金鹏 中国科学院兰州地质研究所兰州730000  
赵欣 中国科学院兰州地质研究所兰州730000  
王琪 中国科学院兰州地质研究所兰州730000  
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摘要:
Triassic Turbidity Current Deposit and Genetic Model of Yanchang Formation of Xifeng Oilfield, Ordos Basin
      Triassic turbidity current deposits of Yanchang Formation well developed in the Xifeng oilfield, Ordos basin. According to the core,well-logging data and outcrop, efforts are made in this thesis to recognize turbidity current channel,pigtail turbidity current channel,layer turbidity current,trough turbidity current and slump turbidity current from strata. Based on the theory of sediment dynamics and mechanism of genetic of turbidity current, two kinds of genetic models of turbidity current are developed: the genetic model of flood turbidity current and the genetic model of slump turbidity current. Then the relationship between turbidity current deposits and tectonic condition is analyzed. This thesis puts forward suggestion that the tectonic setting controls the mode of space-time exhibition of turbidity current deposits.
LU Long-fei,SHI Ji-an,CAI Jin-gong,WANG Jin-peng,ZAHO Xin,WANG Qi.2006.Triassic Turbidity Current Deposit and Genetic Model of Yanchang Formation of Xifeng Oilfield, Ordos Basin[J].Acta Geoscientica Sinica,27(4):303-309.
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