地壳形变与地震
地殼形變與地震
지각형변여지진
CRUSTAL DEFORMATION AND EARTHQUAKE
2001年
2期
70-76
,共7页
张四新%江在森%王双绪%程宏宾
張四新%江在森%王雙緒%程宏賓
장사신%강재삼%왕쌍서%정굉빈
垂直形变%地震活动%祁连山%继承性运动
垂直形變%地震活動%祁連山%繼承性運動
수직형변%지진활동%기련산%계승성운동
基于1972~2000年北祁连-河西地区的垂直形变观测资料,分析研究了该区垂直形变场的演化及其与地震的关系,得到如下结论:①本区构造运动近30年来的演化过程为逆继承性运动-继承性运动增强-持续继承性运动-逆继承性运动-继承性运动这样一个“旋回”过程,继承性运动是构造运动的总趋势;②垂直形变场演化与地震活动强弱存在一定的相关性,但地震活动强弱明显“滞后”于地壳运动;③1995~2000年构造运动恢复继承性运动,且山区与盆地的差异性运动较1989~1995年有所增强,表明本区构造应力场有强化趋势,未来几年祁连构造带中东段有发生中强地震的可能。
基于1972~2000年北祁連-河西地區的垂直形變觀測資料,分析研究瞭該區垂直形變場的縯化及其與地震的關繫,得到如下結論:①本區構造運動近30年來的縯化過程為逆繼承性運動-繼承性運動增彊-持續繼承性運動-逆繼承性運動-繼承性運動這樣一箇“鏇迴”過程,繼承性運動是構造運動的總趨勢;②垂直形變場縯化與地震活動彊弱存在一定的相關性,但地震活動彊弱明顯“滯後”于地殼運動;③1995~2000年構造運動恢複繼承性運動,且山區與盆地的差異性運動較1989~1995年有所增彊,錶明本區構造應力場有彊化趨勢,未來幾年祁連構造帶中東段有髮生中彊地震的可能。
기우1972~2000년북기련-하서지구적수직형변관측자료,분석연구료해구수직형변장적연화급기여지진적관계,득도여하결론:①본구구조운동근30년래적연화과정위역계승성운동-계승성운동증강-지속계승성운동-역계승성운동-계승성운동저양일개“선회”과정,계승성운동시구조운동적총추세;②수직형변장연화여지진활동강약존재일정적상관성,단지진활동강약명현“체후”우지각운동;③1995~2000년구조운동회복계승성운동,차산구여분지적차이성운동교1989~1995년유소증강,표명본구구조응력장유강화추세,미래궤년기련구조대중동단유발생중강지진적가능。
By analyzing the vertical deformation field in 1972~2000 in Hexi area,the following results are obtained:①In recent 30 years,tectogenesis reflected by the vertical deformation field undergoes a ‘cyclic’ evolutive process, i.e. counter-inheritance motion,enhanced inheritance motion,persistent inheritance motion,counter-inheritance motion,inheritance motion.The total trend of this motion is inheritent.②This research shows that the vertical deformation is correlative to seismic activity and the strenthening and weakening of the seismicity lag obviously behind crustal movement.③Tectogenesis resumes inheritance motion in 1995~2000,and diversity motion between mountain and basin was stronger than last period,so there is an intensive trend of tectonic stress field,in a few coming years there is probably middle-strong earthquake in middle-eastern segment of QiLian tectonic zone.