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祁连山与河西走廊近期垂直形变特征

THE CHARACTERISTICS OF RECENT VERTICAL DEFORMATION IN QILIAN MOUNTAIN AND HEXI CORRIDOR

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【作者】 丁平于建民江在森

【Author】 Ding ping Yu Jianmin Jiang Zaisen(Second Seismo-Geodetic brigade, S.S.B.)

【机构】 国家地震局第二测量大队国家地震局第二测量大队

【摘要】 本文用广义逆速率模型及拟稳速率模型处理了祁连山与河西走廊地区近20年来的水准测量资料。研究结果表明:该地区70年代垂直形变曾出现逆继承性;80年代恢复了祁连山上升,走廊盆地沉降的继承性运动,并有强化趋势。

【Abstract】 Using the generalized inverse and substationary rate model, this paper analyses the geodetic levelling data of recent 20 years in Qilian and Hexi area. The research indicates that converse successive movement of crust in this area appeared in 1970’s, and that the movement has returned to normal, which is Qilian mountain upheaving and Hexi corridor subsiding since the end of 1970’s. The authors recognize that the tendency of successive movement is intensifying in 1980’s.

  • 【文献出处】 地壳形变与地震 ,Crustal Deformation and Earthquake , 编辑部邮箱 ,1991年02期
  • 【被引频次】7
  • 【下载频次】56
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