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首页> 外文会议>IASME/WSEAS International Conference on Geology and Seismology >ON THE CONTRADICTORY CHARACTERISTICS OF THE EEP SIGNAL OBSERVED PRIOR TO THE KYTHIRA M 6.9 EARTHQUAKE ON JANUARY 2006
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ON THE CONTRADICTORY CHARACTERISTICS OF THE EEP SIGNAL OBSERVED PRIOR TO THE KYTHIRA M 6.9 EARTHQUAKE ON JANUARY 2006

机译：2006年1月在Kythira M 6.9地震前观察到EEP信号的矛盾特征

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摘要

The continuous operation of the telemetric network of seismoelectromagnetic stations at the southern frontal part of the Hellenic Arc, one of the most active geophysical and seismological laboratories of nature in Europe, has enabled the detection and identification of a number of electric, magnetic and electromagnetic phenomena which have been repeatedly reported as forerunners of earthquakes. Aiming to identify the nature of such signals several models have been proposed based upon the characteristics exhibited by the observed anomalies and different possible generation mechanisms. Most of the observed anomalies appear to coincide with the main characteristics featured by seismic electric signals (SES) and electric earthquake precursors (EEP) which are considered to be the main candidates for short-term earthquake precursors. This paper, though, discusses an electric potential anomaly, captured by electric field recordings, accompanying the Kythira M 6.9 earthquake on the 8th of January, 2006, which exhibits different characteristics to the existing EEP and SES models, and presents the authors' thesis regarding the nature of this particular signal along with a plausible generation mechanism.
机译：Heldenic Arc南部正面部分的地震电信站的遥测网络遥测的连续运行，欧洲最具活跃的地球物理和地震实验室之一，使得检测和识别许多电磁和电磁现象这被一再报告为地震的先行者。旨在识别这些信号的性质，基于观察到的异常和不同可能的产生机制表现出的特征，提出了多种模型。大多数观察到的异常似乎与地震电信号（SES）和电气地震前体（EEP）特征的主要特征一致，其被认为是短期地震前体的主要候选者。然而，本文讨论了由电场录音捕获的电势异常，伴随着Kythira M 6.9地震，于2006年1月8日伴随着现有EEP和SES模型的不同特征，并提出了作者论文这种特定信号的性质以及合理的生成机制。

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