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根据有关电报前后的选定地区的地震学资料,我们重新检查了所有能得到的VAN电报,发现1981年～1985年期间VAN电报与地震的相关性是随机的。任何震级的地震,从非常短距离(如仅几公里)极低阈值(如M=2.5),到大距离(如500 km)中的震级(M=7.0),甚至远震(如1981年伊朗地震,距离约2000 km),被VAN用“表面上的”SES关联起来,这一关联是基于任何地方发生了一次地震(从意大利到爱琴海,从阿尔巴尼亚到希腊的克里特岛)和通常基于VAN研究者之间用以交换的电报。自1986年,大部分VAN电报主要限于欧洲地震活动性最高的希腊西部。分析所有能得到的VAN电报后得出的结论是:VAN预报的没有一个是主震。虽然报道的VAN关联性似乎总是非常令人满意,但所相关的地震不是余震就是相关不唯一,这就意味着同一震中地区的任意地震都可以用电报随意相关。
Based on the seismological data on the selected area before and after the telegraph, we rechecked all available VAN telegrams and found that the correlation between the VAN telegraph and the earthquake was random from 1981 to 1985. Earthquakes of any magnitude, ranging from very low thresholds (eg M = 2.5) over very short distances (eg just a few kilometers) to those over large distances (eg 500 km) (M = 7.0) The earthquakes, at a distance of about 2000 km, are linked by VAN with “superficial” SES based on an earthquake anywhere (from Italy to the Aegean, from Crete to Albania to Greece) and usually Telegraph for exchange based on VAN researchers. Since 1986, most of the VAN cables have been limited mainly to the western part of Greece, the most seismic active in Europe. Analysis of all available VAN telegrams concluded that none of the VAN forecasts were main shocks. Although the reported VAN correlation seems always to be very satisfactory, the associated earthquake is either aftershock or correlated, which means that any earthquake in the same epicenter area can be telepathically associated.