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Lithosphere- Surfacesphere–Atmosphere-Ionosphere Coupling Model for Vrancea Seismic Zone in Romania

机译:罗马尼亚州武装视野地震区的岩石圈 - 表面球 - 气氛 - 电离层耦合模型

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This paper presents a complex multidisciplinary approach concept to explain the nature of short-term earthquake precursors observed in land surface, atmosphere, ionosphere and magnetosphere for strong intermediate depth earthquakes recorded in Vrancea region in Romania. A developed Lithosphere-Surfacesphere-Atmosphere-Ionosphere (LSAI) coupling model can explain most of these presignals as a synergy between different anomalies of geophysical/geochemical parameters. These anomalies prior to medium to strong earthquakes are attributed to the thermodynamic, degassing and ionization processes in the Earth- Atmosphere system and micro-fracturing in the rocks especially along area's active faults. The main outcome of this paper is an unified concept for systematic validation of different types of earthquake precursors of which Land Surface Temperature (LST), outgoing Long wave Radiation (OLR), Surface Latent Heat Flux (SLHF), Air Temperature (AT), radon gas concentration, ionospheric Total Electron Content (TEC) are the most reliable parameters within the chain of the processes described by LSAI model.
机译:本文提出了一种复杂的多学科的方法的概念来解释在土地表面,大气,电离层和磁层观察到在罗马尼亚记录在弗朗恰区域强中间深度的地震短期地震前兆的性质。发达的岩石圈 - 表面苯甲酸薄薄 - 气氛 - 电离层(LSAI)耦合模型可以解释大多数这些教标作为地球物理/地球化学参数不同异常之间的协同作用。这些前介质强震异常归因于在岩石中的地球 ​​- 大气系统和微压裂的热力学,脱气和电离过程特别是沿区域的活动故障。本文的主要结果是一个统一的概念,用于系统验证不同类型的地震前体,其中陆地表面温度(LST),输出长波辐射(OLR),表面潜热通量(SLHF),空气温度(AT),氡气浓度,电离层总电子含量(TEC)是LSAI模型所描述的过程中最可靠的参数。

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