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东亚陆缘新生代盆地的相似性

许浚远

许浚远. 东亚陆缘新生代盆地的相似性[J]. 石油实验地质, 1997, 19(4): 297-304. doi: 10.11781/sysydz199704297
引用本文: 许浚远. 东亚陆缘新生代盆地的相似性[J]. 石油实验地质, 1997, 19(4): 297-304. doi: 10.11781/sysydz199704297
Xu Junyuan. SIMILARITIES BETWEEN CENOZOIC BASINS OF DIFFERENT MAGNITUDES IN EAST ASIA CONTINENTAL MARGIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1997, 19(4): 297-304. doi: 10.11781/sysydz199704297
Citation: Xu Junyuan. SIMILARITIES BETWEEN CENOZOIC BASINS OF DIFFERENT MAGNITUDES IN EAST ASIA CONTINENTAL MARGIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1997, 19(4): 297-304. doi: 10.11781/sysydz199704297

东亚陆缘新生代盆地的相似性

doi: 10.11781/sysydz199704297
基金项目: 国家自然科学基金(49502033)
详细信息
    作者简介:

    许浚远,男,36岁,副教授、博士,构造地质及石油地质

SIMILARITIES BETWEEN CENOZOIC BASINS OF DIFFERENT MAGNITUDES IN EAST ASIA CONTINENTAL MARGIN

  • 摘要: 东亚陆缘新生代盆地几何特征具有相似性,呈以NNE、NEE至EW向断裂为边界的准菱形。它们形成的运动学具有相似性,形成时两侧块体作近NS向分离。它们形成的动力学具有相似性,形成时区域性最小主应力作近NS向展布。现行的"挤出构造"理论不能解释东亚陆缘诸多的构造现象。

     

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出版历程
  • 收稿日期:  1996-05-23
  • 刊出日期:  1997-10-25

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