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首页> 外文期刊>International Journal of Geosciences >Study on the Seismogenic Mechanism of the Earthquake Mw6.9 in 2014 in the Aegean Sea Seismic Cone
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Study on the Seismogenic Mechanism of the Earthquake Mw6.9 in 2014 in the Aegean Sea Seismic Cone

机译：2014年爱琴海地震锥体Mw6.9地震发生机理研究

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In accordance with the Seismo-Geothermics theory about methods of intracrustal strong earthquake and volcano prediction, we use the ANSS earthquake catalogue from the Northern California earthquake data center and the EMSC earthquake catalogue from the European-Mediterranean Seismological Centre to study the seismic activities of the Turkish Branch Seismic Cone in the Mediterranean Seismic Cone and the following Aegean Sea Seismic Cone, and show reproduction through graphics and animation, the seismogenic process and seismogenic mechanism of the earthquake Mw6.9 on May 24,2014 innorthern Aegean Sea. It was concluded that the energy of strong earthquake of magnitude around7 inAegean Seawas probably from energy transfer and accumulation in deep mantle and incentive lithosphere in the way of wave pattern, and then the strong earthquake occurs suddenly in search of the weak parts of the surface structure. The purpose of this paper is to open a hole in the traditional seismic genesis, and it is beneficial to the further research on the theory and method of earthquake prediction. It is our first attempt to study this case and it needs further examination. In this paper, we divide the Turkish Branch Seismic Cone of the Mediterranean Seismic Cone into 4 tertiary seismic cones, and we show a preliminary seismo-tectonic model of Aegean region. It will be conducive to seismic monitoring and earthquake prediction research inGreece,Turkey,RomaniaandPolandregions. At present, the world’s earthquake prediction has little effect, and it even tends to be not cognitive. Innovative thinking is the only way out.
机译：根据关于地壳内强地震和火山预测方法的地震地热学理论，我们使用北加利福尼亚地震数据中心的ANSS地震目录和欧洲-地中海地震中心的EMSC地震目录来研究该地震的地震活动。地中海地震锥和其后的爱琴海地震锥中的土耳其分支地震锥，并通过图形和动画，2014年5月24日爱琴海北部Mw6.9地震的震源过程和震源机制显示了再现。结论是，爱琴海7级附近的强地震的能量可能是通过波型方式在深层地幔和激励岩石圈中的能量转移和积累，然后在寻找表层结构的薄弱部位时突然发生的。 。本文的目的是为传统的地震成因开辟一个漏洞，有利于对地震预测理论和方法的进一步研究。这是我们研究此案的首次尝试，需要进一步研究。在本文中，我们将地中海地震锥的土耳其分支地震锥分为四个第三级地震锥，并展示了爱琴海地区的初步地震构造模型。它将有助于希腊，土耳其，罗马尼亚和波兰地区的地震监测和地震预测研究。目前，世界地震的预测影响甚微，甚至趋向于无法认知。创新思维是唯一的出路。

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