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走滑构造体系盆山耦合与区带分析
引用本文:刘和甫,李晓清,刘立群,廖群山.走滑构造体系盆山耦合与区带分析[J].现代地质,2004,18(2):139-150.
作者姓名:刘和甫  李晓清  刘立群  廖群山
作者单位:1. 中国地质大学,能源地质系,北京,100083
2. 中国地质大学,能源地质系,北京,100083;胜利油田,东胜精攻石油开发集团有限公司,山东,东营,257100
3. 中国石油化工股份有限公司,勘探开发研究院,北京,100083
4. 中国地质大学,能源地质系,北京,100083;中国石油勘探开发研究院,廊坊分院,河北,廊坊,065007
基金项目:国土资源大调查项目 (DKD2 10 40 110 )
摘    要:走滑构造体系盆山耦合常由于走滑断层弯曲所产生 ,结合油气勘探中盆地—区带—圈闭 3个层次 ,相应地划分为 3类走滑断层 :(1)转换断层为控盆断层 ;(2 )转移断层为控带断层 ;(3)撕裂断层为控藏断层。走滑断层伴生盆地按力学性质可以划分为 :(1)走滑伸展盆地 ;(2 )走滑挤压盆地及 (3)走滑旋转盆地。转移断层可以与裂谷盆地或前陆盆地复合 ,发育断裂互联网络 ,形成雁列褶皱或雁列断块油气区带 ;撕裂断层与低角度正断层或逆冲断层相交时常形成有利圈闭 ,如活板构造等。

关 键 词:转换断层  转移断层  撕裂断层  走滑伸展盆地  走滑挤压盆地  走滑旋转盆地
文章编号:1000-8527(2004)02-0139-12
修稿时间:2004年4月1日

PETROLEUM PLAY ANALYSIS AND STRIKE SLIP SYSTEM BASIN-MOUNTAIN COUPLING
LIU He-fu,LI Xiao-qing.PETROLEUM PLAY ANALYSIS AND STRIKE SLIP SYSTEM BASIN-MOUNTAIN COUPLING[J].Geoscience——Journal of Graduate School,China University of Geosciences,2004,18(2):139-150.
Authors:LIU He-fu  LI Xiao-qing
Institution:LIU He-fu~1,LI Xiao-qing~
Abstract:The bending of the strike slip fault dominated the forming of basin and mountain along the fault. This is so-called strike slip system basin-mountain coupling. The strike slip fault can be divided into three different levels corresponding to the different scales of petroleum exploration targets, such as transform fault dominated the basin forming, transfer fault controlled the play, and tear fault charged the trap. According to the mechanical scenario, the strike slip dominated basins can be divided into three types: (1) transtensional basin; (2) transpressional basin; and (3) transrotational basin. The compound of transfer fault with rift basin or foreland basin can form the linked fault family, which produced the echelon fold or echelon fault block. The echelon fold and echelon fault block controlled the plays. The tear fault intersected with low angle normal fault or thrust fault can form some traps, e.g. trap-door structure trap.
Keywords:transform fault  transfer fault  tear fault  transtensional basin  transpressional basin  transrotational basin
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