THE MECHANISM OF ANOMALY OF CHARGED PARTICLES BEFORE THE EARTHQUAKE

2020 ◽  
Vol 7 (3) ◽  
pp. 72-76
Author(s):  
RUSTAM RAKHIMOV ◽  
◽  
ASATULLA MAKHSUDOV

Some mechanisms are considered in the form of analysis of the propagation and origin of charged particles involved in acting forces in energy transfer processes that lead to a highly deformed seismically active state and create the necessary conditions for the occurrence of an earthquake. The results of monitoring the registration of charged particles of radioactive radiation of the earth’s crust for the purpose of earthquake forecasting are analyzed. During monitoring, responses to the origin of an event - an earthquake-are observed in the behavior of charged particles, which are located on remote parts of the earth’s crust relative to the place where charged particles are registered. In this case, wide horizons of the earth’s crust are involved, where tectonic disturbances are developed, covering not only the deep layers of the earth’s crust, but also the sections that appear in the upper parts. These tectonic disturbances can be considered as through-current channels that facilitate the transfer of energy from great depths. On the earth’s surface, the behavior of charged particles should be considered within the framework of the action of geomagnetic and atmospheric electricity fields. These fields at the earth’s surface are a carrier field that provides a special transfer of not only energy and matter. Thus, the propagation of charged particle flows over considerable distances from the epicenter of earthquakes can be caused by the carrier fields of deep change processes.

Author(s):  
V. M. Makeev ◽  
N. V. Makarova ◽  
T. V. Sukhanova

The article deals with the internal deep structure of the earth's crust of the East European platform and the surface of the mantle lithosphere. The presented charts of the three main layers of the earth's crust — the lower, middle and upper and the surface of the mantle lithosphere — for the first time identified deformation by changing the thickness of the layers. Deformations are compared on all layers that allowed to allot the active center, the main (through) and local (developed in separate layers) areas. The boundaries of these regions are active zones of different ranks. The observed end-to-end development of strain from layer to layer or expression of some of them only in separate layers indicates on the sub-horizontal stratification and vertical divisibility of the earth's crust. Deformations of the deep layers are compared with the latest near-surface platform structures. This made it possible to establish a connection of near-surface deformations with deep ones and to consider the latter as the latest. These studies are relevant for solving fundamental problems of the origin of new structures and a number of practical problems.


Author(s):  
B. А. Iskakov ◽  
◽  
D. Besnosko ◽  
V. V. Zhukov ◽  
T. Kh. Sadykov ◽  
...  

The unresolved problem of traditional seismology to date is the separation from the stream of information recorded by numerous seismic sensors of a strictly defined signal about the approach of a catastrophic earthquake specific in time and space. Such a signal is usually lost against a constant background from a large number of another events. At the turn of the 1980s and 1990s, scientists from the Physics Institute and the Institute of Physics of the Earth developed a preliminary concept for a new promising direction in seismology. Using the signal from elastic vibrations in the acoustic frequency range for earthquake prediction. These signals can be generated by ionization. Ionization is formed at the moment of the passage of high-energy muons through a seismically stressed medium in the deep layers of the earth's crust. It is hoped that this method may be one way to predict earthquakes in the future.


Eos ◽  
2002 ◽  
Vol 83 (19) ◽  
pp. 212
Author(s):  
David Deming

Author(s):  
Vladimir Makeev ◽  
Nataliya Makarova

The object of research is the deformation of the deep layers and the Moho surface the East European platform is identified on the basis of structural analysis thickness of the deep layers of the Earth's crust and of the Moho surface. Initial data - geological and geophysical materials of the lithosphere of the East European platform, the thickness of the lower, middle, and upper layers of the Earth's crust, and the newest structures. Research methods are structural-geodynamic and comparative- tectonic, which allow us to assess the spatial and temporal variability of deep and near-surface deformations. Results. Active centers and relatively passive deformations associated are combined into geodynamic regions, the boundaries of which are zones of structural disagreement. Geodynamic regions are divided into main and secondary. The first is expressed by stable and long-term development, the second - is shown in separate layers of the Earth’s crust. It is established that the protrusions of the mantle lithosphere cause a reduction in the thickness of the layers of the Earth's crust and the formation of the newest trough. The sinking of the mantle lithosphere affects the increase in power in the lower and upper layers and the formation of the newest uplifts. The intermediate layer is considered as a compensation layer. Thinning and thick parts of the individual layers lead to the formation of the newest local trough and uplifts. Thus, the conformal and disconform correlation of deformations of deep layers and the newest structures is a characteristic property of the structure of the platform lithosphere. The sources of deep deformations are extra-platform regional areas of recent tectogenesis and intraplatform local active centers - protrusions and trough of the mantle lithosphere, abnormal thickening and thinning of the Earth's crust layers.


1915 ◽  
Vol 79 (2058supp) ◽  
pp. 382-383
Author(s):  
Alphonse Berget

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