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Ground Tilt Variations in the Klyuchevskoi Volcano Area, Kamchatka

机译:堪察加半岛Klyuchevskoi火山区的地面倾斜变化

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We consider the results of ground tilt observations in the area of Klyuchevskoi Volcano, Kamchatka at the Klyuchi and Apakhonchich stations using photoelectric tiltmeters. An anomalous tilt was recorded during a period of increased activity in the summit crater of Klyuchevskoi Volcano in November 1979. In January and February 1980 three more cases of anomalous tilting before the volcano’s active periods were observed. The tilts exhibit some common kinematic features that are quite consistent with the activity periods. Various disturbing influences were estimated as affecting the observations of tilts related to seismic and volcanic events. For the first time in Kamchatka, the parameters of the five principal elastic-tide waves have been determined. Sea tides exerted an indirect effect on the amplitude factors γ(M2)on the E–W component at both sites to decrease them relative to the global value,γ(M2) = 0.7. We investigated the influence of sea tides on the elastic solid earth tide along the Trans-Kamchatka and Kola traverses. The observed and theoreticalγ(M2) factors at both traverses situated in different geodynamic areas are in approximate agreement.
机译:我们使用光电测斜仪考虑了在Klyuchi和Apakhonchich站的Klyuchevskoi火山,Kamchatka地区的地面倾斜观测结果。 1979年11月在Klyuchevskoi火山的山顶火山口活动增加期间记录到异常倾斜。在观察到火山的活跃期之前,在1980年1月和1980年2月又发生了3次异常倾斜事件。倾斜表现出一些与运动周期非常一致的常见运动学特征。据估计,各种干扰影响影响了与地震和火山事件有关的倾斜观测。在堪察加半岛,这是第一次确定了五个主要弹性潮波的参数。海潮对两个地点的E-W分量上的振幅因子γ(M2)都有间接影响,使它们相对于全局值γ(M2)= 0.7减小。我们调查了海潮对沿横贯堪察加和科拉横断面的弹性固体土潮的影响。位于不同地球动力学区域的两个导线的观测和理论γ(M2)因子大致吻合。

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