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青藏高原伦坡拉盆地晚期构造变形特征及应力机制分析

刘中戎 李祥权

刘中戎, 李祥权. 青藏高原伦坡拉盆地晚期构造变形特征及应力机制分析[J]. 石油实验地质, 2017, 39(6): 819-824. doi: 10.11781/sysydz201706819
引用本文: 刘中戎, 李祥权. 青藏高原伦坡拉盆地晚期构造变形特征及应力机制分析[J]. 石油实验地质, 2017, 39(6): 819-824. doi: 10.11781/sysydz201706819
Liu Zhongrong, Li Xiangquan. Late tectonic deformation characteristics and stress mechanism in Lunpola Basin, Tibet Plateau[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2017, 39(6): 819-824. doi: 10.11781/sysydz201706819
Citation: Liu Zhongrong, Li Xiangquan. Late tectonic deformation characteristics and stress mechanism in Lunpola Basin, Tibet Plateau[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2017, 39(6): 819-824. doi: 10.11781/sysydz201706819

青藏高原伦坡拉盆地晚期构造变形特征及应力机制分析

doi: 10.11781/sysydz201706819
基金项目: 国家自然科学基金(41672110)和国家"十三五"重大专项(2016ZX05027-001)资助。
详细信息
    作者简介:

    刘中戎(1972-),男,高级工程师,从事石油勘探开发研究。E-mail:ktnflzr@163.com。

  • 中图分类号: TE121.2

Late tectonic deformation characteristics and stress mechanism in Lunpola Basin, Tibet Plateau

  • 摘要: 以伦坡拉盆地区域二维地震资料解释为基础,提炼出盆地晚期改造主要存在张扭横向调节构造变形、冲断压陷构造变形、推挤褶隆构造变形和压扭隆起构造变形4种构造变形样式,进而将该盆地"南北分带、东西分区"的构造变形格局划分为10个构造变形分区,即:南部冲断带、南部推挤褶隆带、南部压扭隆升带、北部冲断带、北部推挤褶隆带、西部推挤隆升区、西部冲断压陷区、中部横向张扭调节区、东部冲断压陷区和东部推挤隆升区。压性构造样式与张性构造样式共存且统一于左旋斜向对挤的压性应力场,是伦坡拉盆地晚期构造变形的特征。

     

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出版历程
  • 收稿日期:  2017-08-18
  • 修回日期:  2017-10-20
  • 刊出日期:  2017-11-28

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