ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
含盐前陆充填变形前缘盐上层构造样式
  
关键词:evaporite  foreland  leading edge of deformation  structural style
基金项目:国家自然科学基金项目(编号:40172076),国家重点基础研究发展规划项目(编号:G19990433)
作者单位
陈书平 石油大学石油天然气成藏机理教育部重点实验室北京102249
石油大学盆地与油藏研究中心北京102249 
汤良杰 石油大学石油天然气成藏机理教育部重点实验室北京102249
石油大学盆地与油藏研究中心北京102249 
贾承造 中国石油天然气股份有限公司北京100011 
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摘要:
Structural Styles in the Deformation Leading Edge of Evaporite-bearing Foreland Basin Fill
      Structural styles and their relationships in thedeformation leadingedge of the evaporite-bearing foreland basin fill are discussed based on the thickness of the evaporite layer and its overburden. The basic structural styles of the overburden, i.e., fold or fault, are determined by the relative thicknessbetween the overburden and the evaporite layer. Where the area in core of a detachment fold is smaller than or equal to the area of evaporite available to supply core of the fold, an anticline will form. Where the area in core of a detachment fold is larger than the area of the evaporite available to supply core of thefold, faults will form. As for the la-ter, the structural styles are controlledby the intersection position of two back thrust faults. Where two back thrust faults intersect within or under the evaporite layer, a pop-up will form. Where two back thrust faults intersect within the overburden, a pop-up will form abovethe intersection and a triangle with partial overburden sequence will form underthe intersection. Where two back thrust faults intersect above the overburden, atriangle zone with a complete overburden sequence will form. The position of the intersection is determined by the thickness of the overburden.
CHEN Shu-ping,TANG Cheng-jie,JIA Cheng-zao.2004.Structural Styles in the Deformation Leading Edge of Evaporite-bearing Foreland Basin Fill[J].Acta Geoscientica Sinica,25(5):561-564.
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