陈绍绪, 朱学武. 邯郸地区地壳形变的研究[J]. 华北地震科学, 1987, 5(1): 42-50.
引用本文: 陈绍绪, 朱学武. 邯郸地区地壳形变的研究[J]. 华北地震科学, 1987, 5(1): 42-50.
Chen Shaoxu, Zhu Xuewu. STUDY OF THE CRUSTAL DEFORMATION IN HANDAN AREA[J]. North China Earthquake Sciences, 1987, 5(1): 42-50.
Citation: Chen Shaoxu, Zhu Xuewu. STUDY OF THE CRUSTAL DEFORMATION IN HANDAN AREA[J]. North China Earthquake Sciences, 1987, 5(1): 42-50.

邯郸地区地壳形变的研究

STUDY OF THE CRUSTAL DEFORMATION IN HANDAN AREA

  • 摘要: 河北省邯郸地区与山东、河南和山西接壤,属于晋、冀、鲁、豫交界地区。这一地区多年来被列入全国重点监视区之一。近年来在这一地区进行多次精密水准测量,发现了一些重大的异常变化。有必要对这些变化进行认真研究。

     

    Abstract: This paper has investigated sevreal places where vertical deformations are significant in Handan area, It has been considered that the rapid subsidence at Feixang in recnet years may be a result of greatly pumping groundwater.The leveling data of Hanbau area reveal the up-to-date activity of Taihang mountain piedmont fault. The mode of the activity is successional, the east wall of the Taihang mountain piedmont fault is sinking as compaed with the west one Tht rates of the activity are 6mm/yin Yongnian, 4.7mm/y in Handan city and 1.8mm/y in Cixan respectively.The results of leveling survey also reflect the activity of Gushan-Zishan fault.Wuan basin lying to the west side of Gushan-Zishan far, It is sinking as compared with the Gushan upheaval in tht east. The leveling line crossing Gushan-Zishan fault tilted 4. lurad down to the west in the period 1980-1984.

     

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