杨裕利. 运用地貌学方法研究平原地区隐伏断裂——以大同盆地内部NE向隐伏断裂为例[J]. 武汉大学学报 ( 信息科学版), 1986, 11(2): 65-75.
引用本文: 杨裕利. 运用地貌学方法研究平原地区隐伏断裂——以大同盆地内部NE向隐伏断裂为例[J]. 武汉大学学报 ( 信息科学版), 1986, 11(2): 65-75.
shu
Yang Yuli. The Application of Geomorphology to the Study of Invisible Active Faults in Plains——taking the invisible active faults (NE) in the Datong Basin for example[J]. Geomatics and Information Science of Wuhan University, 1986, 11(2): 65-75.
Citation: Yang Yuli. The Application of Geomorphology to the Study of Invisible Active Faults in Plains——taking the invisible active faults (NE) in the Datong Basin for example[J]. Geomatics and Information Science of Wuhan University, 1986, 11(2): 65-75.
shu

运用地貌学方法研究平原地区隐伏断裂——以大同盆地内部NE向隐伏断裂为例

The Application of Geomorphology to the Study of Invisible Active Faults in Plains——taking the invisible active faults (NE) in the Datong Basin for example

    摘要
  • 摘要: 运用地貌学方法,对河流阶地的研究,是探索平原区隐伏活动断裂的有效方法之一。依据实测河流阶地(御河,十里河,鹅毛口河,大峪河)的数据作横剖面图,阶地位相图和通过钻探资料的分析,证实有两条NE向隐伏断裂的存在,并在其控制下形成地垒,地垒构造至今还在活动。

     

    Abstract: The application of geomorphology to the study of river terraces is one of the most effective ways to search for the invisible active faults in plains. This paper analyzes the cross-section and facies maps drawn on the basis of the data from the survey of the terraces of Yu River, Shill River, Emaokou River, and Dayu River as well as the drilling data, proving the existence of two invisible faults (NE) and an active horst formed under their control.

     

    • HTML全文
    • 参考文献(0)
    • 相关文章
    • 施引文献
  • 资源附件(0)

/

返回文章
返回