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Low-frequency emissions and related phenomena in the ionosphere above the lithosphere deep faults inferred from satellite data

机译:根据卫星数据推断的岩石圈以上深层电离层的低频辐射及相关现象

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The comparative analysis of the variations of the low-frequency emission (0.1-20 kHz) intensity, low-energy electron fluxes and the plasma temperature at satellite altitudes (on 10 orbits of the "Intercosmos 19" satellite) above the lithosphere deep faults of the Norwegian Sea, the Baltic Shield, the Barents-Kara shelf and the West-Sibirian Lowland has been carried out. All these regions represent consistent changes in the Earth crustal structure and its geodynamic characteristics in the zone of transition from the Euroasian continent to the Arctic Ocean. The tectonic structures of these regions have different physical parameters and seismic activity. It has been detected that a special character of the low-frequency electromagnetic emission characterises each type of the lithosphere structure. (C) 2006 Elsevier Ltd. All rights reserved.
机译:岩石圈深部断层以上卫星高度(“ Intercosmos 19”卫星的10个轨道上)的卫星高度处的低频发射(0.1-20 kHz)强度,低能电子通量和等离子体温度变化的比较分析。挪威海,波罗的海盾,Barents-Kara陆架和西西比里安低地已经开展。所有这些区域代表着从欧陆大陆到北冰洋过渡带的地壳结构及其地球动力学特征的持续变化。这些地区的构造结构具有不同的物理参数和地震活动。已经检测到低频电磁发射的特殊特征表征了岩石圈结构的每种类型。 (C)2006 Elsevier Ltd.保留所有权利。

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