The Hypothesis of the Relationship Between the Current Seismic Process and the Geomagnetic Field Pulsations

With respect to the increased frequency of the seismic activity symptoms and their disastrous aftereffects and taking into account the publications devoted to severe earthquakes in the Antarctics (1998), Kaliningrad oblast (2004), China (2008), Kirghizia (2008), South Pakistan (2008) and other place...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Datum:2009
Hauptverfasser: Brodsky, Yu.B., Gannoshyn, V.P.
Format: Artikel
Sprache:English
Veröffentlicht: Національний антарктичний науковий центр МОН України 2009
Schriftenreihe:Український антарктичний журнал
Schlagworte:
Online Zugang:http://dspace.nbuv.gov.ua/handle/123456789/128557
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
Назва журналу:Digital Library of Periodicals of National Academy of Sciences of Ukraine
Zitieren:The Hypothesis of the Relationship Between the Current Seismic Process and the Geomagnetic Field Pulsations / Yu.B. Brodsky, V.P. Gannoshyn // Український антарктичний журнал. — 2009. — № 8. — С. 120-125. — Бібліогр.: 8 назв. — англ.

Institution

Digital Library of Periodicals of National Academy of Sciences of Ukraine
id irk-123456789-128557
record_format dspace
spelling irk-123456789-1285572018-01-12T03:03:02Z The Hypothesis of the Relationship Between the Current Seismic Process and the Geomagnetic Field Pulsations Brodsky, Yu.B. Gannoshyn, V.P. Геолого-геофізичні дослідження With respect to the increased frequency of the seismic activity symptoms and their disastrous aftereffects and taking into account the publications devoted to severe earthquakes in the Antarctics (1998), Kaliningrad oblast (2004), China (2008), Kirghizia (2008), South Pakistan (2008) and other places, the paper presents the analysis of the influence of the seismic process on the effects in the circumterrestrial plasma. The authors propose a new hypothesis of the relationship in the lithosphere – geomagnetic field system which is based on the interaction between the moving tectonic plates and the Earth's magnetic field. В связи с участившимися случаями проявления сейсмической активности и их катастрофическими последствиями, с учетом опубликованных материалов о сильных землетрясениях в Антарктиде (1998 год), Калининградской области (2004 год), Китае (2008 год), Киргизии (2008 год), Южном Пакистане (2008 год) и многих других представлен анализ влияния сейсмического процесса на эффекты в околоземной плазме. Предложена новая гипотеза связи в системе литосфера–геомагнитное поле, основанная на взаимодействии движущихся тектонических плит с магнитным полем Земли. 2009 Article The Hypothesis of the Relationship Between the Current Seismic Process and the Geomagnetic Field Pulsations / Yu.B. Brodsky, V.P. Gannoshyn // Український антарктичний журнал. — 2009. — № 8. — С. 120-125. — Бібліогр.: 8 назв. — англ. 1727-7485 http://dspace.nbuv.gov.ua/handle/123456789/128557 550.348.0985:551.14á en Український антарктичний журнал Національний антарктичний науковий центр МОН України
institution Digital Library of Periodicals of National Academy of Sciences of Ukraine
collection DSpace DC
language English
topic Геолого-геофізичні дослідження
Геолого-геофізичні дослідження
spellingShingle Геолого-геофізичні дослідження
Геолого-геофізичні дослідження
Brodsky, Yu.B.
Gannoshyn, V.P.
The Hypothesis of the Relationship Between the Current Seismic Process and the Geomagnetic Field Pulsations
Український антарктичний журнал
description With respect to the increased frequency of the seismic activity symptoms and their disastrous aftereffects and taking into account the publications devoted to severe earthquakes in the Antarctics (1998), Kaliningrad oblast (2004), China (2008), Kirghizia (2008), South Pakistan (2008) and other places, the paper presents the analysis of the influence of the seismic process on the effects in the circumterrestrial plasma. The authors propose a new hypothesis of the relationship in the lithosphere – geomagnetic field system which is based on the interaction between the moving tectonic plates and the Earth's magnetic field.
format Article
author Brodsky, Yu.B.
Gannoshyn, V.P.
author_facet Brodsky, Yu.B.
Gannoshyn, V.P.
author_sort Brodsky, Yu.B.
title The Hypothesis of the Relationship Between the Current Seismic Process and the Geomagnetic Field Pulsations
title_short The Hypothesis of the Relationship Between the Current Seismic Process and the Geomagnetic Field Pulsations
title_full The Hypothesis of the Relationship Between the Current Seismic Process and the Geomagnetic Field Pulsations
title_fullStr The Hypothesis of the Relationship Between the Current Seismic Process and the Geomagnetic Field Pulsations
title_full_unstemmed The Hypothesis of the Relationship Between the Current Seismic Process and the Geomagnetic Field Pulsations
title_sort hypothesis of the relationship between the current seismic process and the geomagnetic field pulsations
publisher Національний антарктичний науковий центр МОН України
publishDate 2009
topic_facet Геолого-геофізичні дослідження
url http://dspace.nbuv.gov.ua/handle/123456789/128557
citation_txt The Hypothesis of the Relationship Between the Current Seismic Process and the Geomagnetic Field Pulsations / Yu.B. Brodsky, V.P. Gannoshyn // Український антарктичний журнал. — 2009. — № 8. — С. 120-125. — Бібліогр.: 8 назв. — англ.
series Український антарктичний журнал
work_keys_str_mv AT brodskyyub thehypothesisoftherelationshipbetweenthecurrentseismicprocessandthegeomagneticfieldpulsations
AT gannoshynvp thehypothesisoftherelationshipbetweenthecurrentseismicprocessandthegeomagneticfieldpulsations
AT brodskyyub hypothesisoftherelationshipbetweenthecurrentseismicprocessandthegeomagneticfieldpulsations
AT gannoshynvp hypothesisoftherelationshipbetweenthecurrentseismicprocessandthegeomagneticfieldpulsations
first_indexed 2025-07-09T09:19:54Z
last_indexed 2025-07-09T09:19:54Z
_version_ 1837160514062385152
fulltext THE HYPOTHESIS OF THE RELATIONSHIP BETWEEN THE CURRENT SEISMIC PROCESS AND THE GEOMAGNETIC FIELD PULSATIONS Yu.B. Brodsky, V.P. Gannoshyn Zhitomir National Agroecological University, 7 Stary bulvar, 10008 Zhitomir, e-mail: YBrodskiy@academy.zt.ua The hypothesis of the relationship between the current seismic process and the geomagnetic field pulsations by Yu.B. Brodsky, V.P. Gannoshyn Abstract. With respect to the increased frequency of the seismic activity symptoms and their disastrous aftereffects and taking into account the publications devoted to severe earthquakes in the Antarctica (1998), Kaliningrad oblast (2004), China (2008), Kirghizia (2008), South Pakistan (2008) and other places, the paper presents the analysis of the influence of the seismic process on the effects in the circumterrestrial plasma. The authors propose a new hypothesis of the relationship in the lithosphere – geomagnetic field system which is based on the interaction between the moving tectonic plates and the Earth's magnetic field. Alongside with the seismic process development the linear velocity of the tectonic plate deformation is increasing which results in the change in the shape of the geomagnetic field intensity line, which, though elastic, is trying to take its initial shape. The changes in the shape of the geomagnetic field intensity line bring about the appearance of the oscillation process of the latter (the so-called stationary wave). In the critical moment of time, when the rock reaches its ultimate stress limit, one can observe the discontinuity or the Earth's crust fault which is accompanied by a rapid increase in the oscillation amplitude of the force geomagnetic line. The paper also presents the results of modelling the pulsations of the geomagnetic field Z-component, the above testifying to a direct relationship and the disturbance of the Earth's magnetic field. The estimates obtained are nicely coordinated with the results of geomagnetic field pulsation measurements which were carried out on the Academician Vernadsky station before the severe crust thearthquake in the Antarctics on the 25 of March 1998 (Bakhmutov, Sedova, Mozgovaya, 2003). Key words: acoustic and gravitation waves, earthquake, Earth's magnetic field, pulsations of the geomagnetic force line Z-component. Ðåôåðàò.  ñâÿçè ñ ó÷àñòèâøèìèñÿ ñëó÷àÿìè ïðîÿâëåíèÿ ñåéñìè÷åñêîé àêòèâíîñòè è èõ êàòàñòðîôè÷åñêèìè ïîñëåäñòâèÿìè, ñ ó÷åòîì îïóáëèêîâàííûõ ìàòåðèàëîâ î ñèëüíûõ çåìëåòðÿñåíèÿõ â Àíòàðêòèäå (1998 ãîä), Êàëèíèíãðàäñêîé îáëàñòè (2004 ãîä), Êèòàå (2008 ãîä), Êèðãèçèè (2008 ãîä), Þæíîì Ïàêèñòàíå (2008 ãîä) è ìíîãèõ äðóãèõ ïðåäñòàâëåí àíàëèç âëèÿíèÿ ñåéñìè÷åñêîãî ïðîöåññà íà ýôôåêòû â îêîëîçåìíîé ïëàçìå. Ïðåäëîæåíà íîâàÿ ãèïîòåçà ñâÿçè â ñèñòåìå ëèòîñôåðà–ãåîìàãíèòíîå ïîëå, îñíîâàííàÿ íà âçàèìîäåéñòâèè äâèæóùèõñÿ òåêòîíè÷åñêèõ ïëèò ñ ìàãíèòíûì ïîëåì Çåìëè. Ïî ìåðå ðàçâèòèÿ ñåéñìè÷åñêîãî ïðîöåññà óâåëè÷èâàåòñÿ ëèíåéíàÿ ñêîðîñòü äåôîðìàöèè òåêòîíè÷åñêîé ïëèòû, ÷òî ïðèâîäèò ê èçìåíåíèþ ôîðìû ñèëîâîé ëèíèè ãåîìàãíèòíîãî ïîëÿ, êîòîðàÿ, îáëàäàÿ óïðóãîñòüþ, ñòðåìèòñÿ ïðèíÿòü ñâîþ ïåðâîíà÷àëüíóþ ôîðìó. Èçìåíåíèå ôîðìû ñèëîâîé ëèíèè ãåîìàãíèòíîãî ïîëÿ ïðèâîäèò ê âîçíèêíîâåíèþ êîëåáàòåëüíîãî ïðîöåññà ïîñëåäíåé (ñòîÿ÷àÿ âîëíà).  êðèòè÷åñêèé ìîìåíò âðåìåíè, êîãäà äîñòèãàåòñÿ ïðåäåë íàïðÿæåíèÿ ïðî÷íîñòè ïîðîä, ïðîèñõîäèò íàðóøåíèå ñïëîøíîñòè, èëè ðàçðûâ, çåìíîé êîðû ñ ðåçêèì óâåëè÷åíèåì àìïëèòóäû êîëåáàíèé ñèëîâîé ã å î ì à ã í è ò í î é ë è í è è . Ï ð å ä ñ ò à â ë å í û ð å ç óë üò à ò û ì î ä å ë è ð î â à í è ÿ ï óë ü ñ à ö è é Z-ñîñòàâëÿþùåé ãåîìàãíèòíîãî ïîëÿ, ïîäòâåðæäàþùèå ïðÿìóþ ñâÿçü ìåæäó ïðîòåêàþùèì ñåéñìè÷åñêèì ïðîöåññîì è âîçìóùåíèåì ìàãíèòíîãî ïîëÿ Çåìëè. Ïîëó÷åííûå îöåíêè õîðîøî ñîãëàñóþòñÿ ñ ðåçóëüòàòàìè èçìåðåíèé ïóëüñàöèé ãåîìàãíèòíîãî ïîëÿ íà ñòàíöèè Àêàäåìèê Âåðíàäñêèé ïåðåä ñèëüíûì êîðîâûì çåìëåòðÿñåíèåì â Àíòàðêòèäå 25 ìàðòà 1998 ãîäà (Áàõìóòîâ, Ñåäîâà, Ìîçãîâàÿ, 2003). Êëþ÷åâûå ñëîâà: àêóñòè÷åñêèå è ãðàâèòàöèîííûå âîëíû, çåìëåòðÿñåíèå, ìàãíèòíîå ïîëå Çåìëè, ïóëüñàöèè Z-ñîñòàâëÿþùåé ãåîìàãíèòíîãî ïîëÿ ÓÊÐÀ¯ÍÑÜÊÈÉ ÀÍÒÀÐÊÒÈ×ÍÈÉ ÆÓÐÍÀË ÓÀÆ ¹ 8, 120-125 (2009) ÓÄÊ 550.348.0985:551.14á 120 121 óïîòåçà çâ'ÿçêó ñåéñì³÷íîãî ïðîöåñó ç ïóëüñàö³ÿìè ãåîìàãí³òíîãî ïîëÿ. Þ.Á. Áðîäñüêèé, Â.Ï. Ãàííîøèí Ðåôåðàò. Ó çâ'ÿçêó ç âèïàäêàìè ïðîÿâó ñåéñì³÷íî¿ àêòèâíîñò³, ùî ïî÷àñò³øàëè, òà ¿õ êàòàñòðîô³÷íèìè íàñë³äêàìè, ç óðàõóâàííÿì îïóáë³êîâàíèõ ìàòåð³àë³â ïðî ñèëüí³ çåìëåòðóñè â Àíòàðêòèä³ (1998 ð³ê), Êàë³í³íãðàäñüê³é îáëàñò³ (2004 ð³ê), Êèòà¿ (2008 ð³ê), Êèðãè糿 (2008 ð³ê), ϳâäåííîìó Ïàêèñòàí³ (2008 ð³ê) é áàãàòüîõ ³íøèõ ïðåäñòàâëåíî àíàë³ç âïëèâó ñåéñì³÷íîãî ïðîöåñó íà åôåêòè â íàâêîëîçåìí³é ïëàçì³. Çàïðîïîíîâàíî íîâó ã³ïîòåçó çâ'ÿçêó â ñèñòåì³ ë³òîñôåðà–ãåîìàãí³òíå ïîëå, çàñíîâàíó íà âçàºìî䳿 ðóõîìèõ òåêòîí³÷íèõ ïëèò ç ìàãí³òíèì ïîëåì Çåìë³.  ì³ðó ðîçâèòêó ñåéñì³÷íîãî ïðîöåñó çá³ëüøóºòüñÿ ë³í³éíà øâèäê³ñòü äåôîðìàö³¿ òåêòîí³÷íî¿ ïëèòè, ùî ïðèçâîäèòü äî çì³íè ôîðìè ñèëîâî¿ ë³í³¿ ãåîìàãí³òíîãî ïîëÿ, ÿêà, ìàþ÷è ïðóæí³ñòü, ïðàãíå ïðèéíÿòè ñâîþ ïåðâèííó ôîðìó. Çì³íà ôîðìè ñèëîâî¿ ë³í³¿ ãåîìàãí³òíîãî ïîëÿ âèêëèêຠâèíèêíåííÿ êîëèâàëüíîãî ïðîöåñó îñòàííüî¿ (ñòîÿ÷à õâèëÿ). Ó êðèòè÷íèé ìîìåíò ÷àñó, êîëè äîñÿãàºòüñÿ ìåæà íàïðóãè ì³öíîñò³ ïîð³ä, â³äáóâàºòüñÿ ïîðóøåííÿ ñóö³ëüíîñò³, àáî ðîçðèâ, çåìíî¿ êîðè ç ð³çêèì çá³ëüøåííÿì àìïë³òóäè êîëèâàíü ñèëîâî¿ ãåîìàãí³òíî¿ ë³í³¿. Ïðåäñòàâëåíî ðåçóëüòàòè ìîäåëþâàííÿ ïóëüñàö³é Z-ñêëàäîâî¿ ãåîìàãí³òíîãî ïîëÿ, ÿê³ ï³äòâåðäæóþòü ïðÿìèé çâ'ÿçîê ì³æ ïðîò³êàþ÷èì ñåéñì³÷íèì ïðîöåñîì ³ çáóðåííÿì ìàãí³òíîãî ïîëÿ Çåìë³. Îòðèìàí³ îö³íêè äîáðå óçãîäæóþòüñÿ ç ðåçóëüòàòàìè âèì³ðþâàíü ïóëüñàö³é ãåîìàãí³òíîãî ïîëÿ íà ñòàíö³¿ Àêàäåì³ê Âåðíàäñüêèé ïåðåä ñèëüíèì êîðîâèì çåìëåòðóñîì â Àíòàðêòèä³ 25 áåðåçíÿ 1998 ðîêó (Áàõìóòîâ, Ѻäîâà, Ìîçãîâà, 2003). Êëþ÷îâ³ ñëîâà: àêóñòè÷í³ òà ãðàâ³òàö³éí³ õâèë³, çåìëåòðóñ, ìàãí³òíå ïîëå Çåìë³, ïóëüñàö³¿ Z-ñêëàäîâî¿ ãåîìàãí³òíîãî ïîëÿ 1. Introduction One of the most important problems of ecological safety connected with the modern prediction of the coming earthquake still remains unsolved. Catastrophic after-effects of this natural phenomenon put forward a task of informative earthquake forerunners search. Such task presupposes exposure of different geophysical effects arising during seismic process, their further interpretation with the aim of new prediction method development. Earthquake is a rather lasting process which is accompanied by different geophysical phenomena, manifesting themselves not only in bowels of the earth, separate parts of lithosphere, but in hydrosphere, biosphere, atmosphere, including bits upper layers – ionosphere. That is why earthquake should be considered as an event that leads to the misbalance in the system of connected Earth forms and near-Earth area. Up to now two opposite views of the researchers have been formed as for the forerunners of the coming earthquake. The first one is based on the fact that the earthquake source is in the earth's crust, the second one is based on the fact that the earthquake source is the geophysical influence of Sun and interplanetary magnetic field. In this connection the authors focused their investigations on the explanation of the hypothesis suggested – the interaction between the moving tectonic plates and pulsation of geomagnetic field before and during earthquake. 2. Short analysis of known interaction hypothesis in the system lithosphere- atmosphere- ionosphere We'll consider and analyze the known hypothesis in the system lithosphere-atmosphere- ionosphere in the preparation period and earthquake origin (Ëèïåðîâñêèé, 2006). Alongside it is necessary to take into account that up to now there is no generally accepted physical model of interconnection between the seismic process and phenomena in the near-earth cosmic space. “Echo” hypothesis of electromagnetic interconnection in the system lithosphere-ionosphere presupposes that transmittance of electromagnetic energy from lithosphere into ionosphere, heating and further effecting E-area takes place while stimulating hypothetic resonator in the system ïðîò³êàþ÷îãî Yu.B. Brodsky: THE HYPOTHESIS OF THE RELATIONSHIP BETWEEN THE CURRENT... 122 lithosphere- ionosphere. However there is no experimental prove testifying the benefit of “echo” model. That is why, knowing about the possibility of resonance ionosphere effect manifestation, we can presuppose that these effects are not crucial in lithosphere-ionosphere interconnection. “Acoustics-gravitation” hypothesis. According to this hypothesis atmosphere acoustics- gravitational waves (AGW) are generated in the area of earthquake origin near the earth surface, which are spread through atmosphere reaching the ionosphere tops lead to ionosphere disturbance due to the collision of ions and neutral molecules. AGW generation can be connected with reciprocating movement of earth's crust having block structure with non-stable heat anomalies caused by hothouse gases going out into the atmosphere of earth's crust breaking zones, as well as with non-stable entrance of lithosphere gas masses into atmosphere. The process of AGW generation has not been investigated experimentally yet. The hypothesis of “lithosphere-ionosphere relationship” is based on the effect of radioactivity and transmittance increase, that leads to the “modification of quasi-stable electric field” in the near- earth layer of the atmosphere. However, it is impossible to explain the increase of the maximum layer F2 height and decrease of the electron concentration maximum value within a day before earthquake in the framework of the hypothesis suggested. “Acoustic-electric” hypothesis of the disturbance of Es-generators and mini-current systems in the night E-area of ionosphere under the influence of acoustic impulses coming from the earth is one of the last hypotheses not confirmed by observations. The latter explains effects of ionosphere at rather short distances within several hundreds kilometers from the future epicenter, according to this hypothesis the existence of acoustic impulses is presupposed, they spread from the area of earthquake preparation to ionosphere height and generating electric current in sporadical layers. According to “gravitation-electrostatic” hypothesis impulsive radon isolation takes place in the area of earthquake preparation. If aerosol provided, Freckle local electro gravitational generators and mini-current systems appear for several minutes and horizontally for the ten of meters. Non- stationary charge distribution and creation of mini-current system in separate elements, on the one hand, lead to the splash of infra-red radiation, and, on the other hand, to the transmittance of corresponding disturbance upward into ionosphere. Proceeding from the existing hypothesis, it is possible to suppose, that in the period of seismic process appearance and development a complex of different physical mechanisms are in action, that leads to the corresponding geophysical effects, consideration of which can give a wide range of earthquake forerunners. 3. Hypothesis of lithosphere-geomagnetic field relationship Any earthquake appears as a result of a sudden release of a considerable number of energy in some volume inside the Earth. As a rule, in some earth areas destruction and some other irreversible rock deformation. Proceeding from theoretical preconditions based on “the theory of elastic output” (Reid, 1911), rotation model of earthquake origin, in case of the irregular turning blocks chain with friction (Âèêóëèí, Áûêîâ, Ëóíåâà, 2000), caused by “freezing in” line of force of the geomagnetic field in earth substance (Áî÷êàðåâ, 1985) and the latter “freezing in” ionosphere (Ôèçèêà êîñìîñà. Ìàëåíüêàÿ ýíöèêëîïåäèÿ, 1986), the hypothesis of tectonic slabs deformation influence on the amplitude change of Z-component in the Earth magnetic field lies in the following. At the initial moment (the moment of seismic process origin) the stretching power begins to influence the element of geomagnetic line of force, situated in the Earth's crust from the side of deforming tectonic blocks. The other end of geomagnetic line of force is fixed. The stretching power is slowly increasing in time from 0 till its critical value – ô the break time of homogenic tectonic blocks. êð Prolongation of geomagnetic line of force (geomagnetic line of force possesses elasticity), Yu.B. Brodsky: THE HYPOTHESIS OF THE RELATIONSHIP BETWEEN THE CURRENT... geomagnetic line of force tends to become straight. The attempt to take its original form on the side of geomagnetic line of force leads to the fact that variations appear in every point of geomagnetic line of force length. At the moment of ô time tension of rock strength reaches its strength limit, the rock break will êð occur. In its turn it will lead to the following, on the break side there will be a hit on the geomagnetic line of force, as the result of it a firm wave will spread with big amplitude of hesitation, than before ô êð time. 4.Modelling the relationship of the current seismic process and geomagnetic pulsations Within the framework of the hypothesis suggested we'll consider the behavior of Z-component of Earth geomagnetic field as a function of distance õ (m) from earthquake epicenter along the magnetic line of force, time t (day) from the moment of seismic process origin and height h (km) from earth surface. In this connection we'll consider the wave equation – equation of string hesitation: (1) where T – tension on all string points; ñ – linear sting density. Equation solving (1) using Furrier method, meeting a combination of exceeding and initial conditions usually looks in such a way (Ïèñêóíîâ, 1985): (2) where A string form f (x) is a form of geomagnetic line of force, the speed function ? (õ) is a linear speed of tectonic blocks deformation. The results of modeling the amplitude of pulsations Z(x, t, h), the component of the earth geomagnetic field, as a result of seismic process for maximum atmosphere model (Èñàåâ, Ïóäîâêèí, 1972) and magnitude Ì = 5,0 points are shown in the picture. 123 , 2 2 2 2 2 1 t Z x Z a ¶ ¶ = ¶ ¶ Yu.B. Brodsky: THE HYPOTHESIS OF THE RELATIONSHIP BETWEEN THE CURRENT... r T a =2 1 ; 124 Picture. Dynamics of the development of Z-component geomagnetic field pulsation. Yu.B. Brodsky: THE HYPOTHESIS OF THE RELATIONSHIP BETWEEN THE CURRENT... 125 Conclusions Within the framework of the hypothesis suggested and the results given modeling of the geomagnetic field response to the current seismic process it is possible to make several conclusions: 1. At the initial moment of seismic process origin tectonic block undergoes deformation that must lead to the form change of geomagnetic force line. However, insufficiency of power effect from the side of deforming tectonic block on the element of geomagnetic force line, which is in earth's crust, does not contribute to the development of the geomagnetic field wave process. 2. As the seismic process develops the speed of tectonic block deformation increases. On the th25 day of seismic process the peak outlet of tectonic block deformation linear speed takes place alongside with loading decrease without breaking earth integrity with the further increase of tectonic block deformation linear speed. The increase of the latter leads to the change of geomagnetic force line form. Possessing strength geomagnetic force line tends to take the initial form, that as a result causes a standing wave along geomagnetic force line (pulsation of geomagnetic field Z – component). th th3. On the 30 and 50 day tectonic block deformation linear speed suddenly increases, earthquake or the outlet of accumulated tensions takes place, which occurs as a result of non-stable deformation localization. Amplitude of pulsation of geomagnetic field Z-component during thearthquake (50 day) is from 420 till 500 mkm. 4. The given results of modeling pulsation of geomagnetic field Z-component confirm the relationship between the seismic process and earth magnetic field. The results obtained accord with the results of measuring pulsations of geomagnetic field at the station of Academician Vernadsky, which preceded the strongest earthquake in Antarktida on March 25, 1998 (Áàõìóòîâ, Ñåäîâà, Ìîçãîâàÿ, 2003). Literature Áî÷êàðåâ Í.Ã. Ìàãíèòíûå ïîëÿ â êîñìîñå. – Ì.: Íàóêà. Ãëàâíàÿ ðåäàêöèÿ ôèçèêî- ìàòåìàòè÷åñêîé ëèòåðàòóðû, 1985. – 208 c. Áàõìóòîâ Â.Ã., Ñåäîâà Ô.È., Ìîçãîâàÿ Ò.À. Ìîðôîëîãè÷åñêèå ïðèçíàêè â ñòðóêòóðå ãåîìàãíèòíûõ âàðèàöèé â ïåðèîä ïîäãîòîâêè ñèëüíåéøåãî çåìëåòðÿñåíèÿ 25 ìàðòà 1998 ã. â Àíòàðêòèäå // Óêðà¿íñüêèé àíòàðêòè÷íèé æóðíàë. – 2003. – ¹ 1. – Ñ. 54–60. Âèêóëèí À.Â., Áûêîâ Â.Ã., Ëóíåâà Ì.Í. Íåëèíåéíûå âîëíû äåôîðìàöèè â ðîòàöèîííîé ìîäåëè ñåéñìè÷åñêîãî ïðîöåññà // Âû÷èñëèòåëüíûå òåõíîëîãèè. – 2000. – Ò. 5. – ¹ 1. – Ñ. 31–39. Èñàåâ Ñ.È., Ïóäîâêèí Ì.È. Ïîëÿðíûå ñèÿíèÿ è ïðîöåññû â ìàãíèòîñôåðå Çåìëè. – Ë.: Íàóêà, 1972. – 244 ñ. Ëèïåðîâñêèé Â.À. Ôèçè÷åñêèå ìîäåëè ñâÿçè â ñèñòåìå ëèòîñôåðà–àòìîñôåðà– èîíîñôåðà: Ëåêöèè ÁØÔÔ – 2006. – Ñ. 58–65.– http://bsfp.iszf.irk.ru/bsfp2006/proceed2006/58- 65.pdf Ïèñêóíîâ Í.Ñ. Äèôôåðåíöèàëüíîå è èíòåãðàëüíîå èñ÷èñëåíèÿ äëÿ âòóçîâ: Ó÷åáíîå ïîñîáèå äëÿ âòóçîâ. – Ò. 2. – 13-å èçä. – Ì.: Íàóêà. Ãëàâíàÿ ðåäàêöèÿ ôèçèêî-ìàòåìàòè÷åñêîé ëèòåðàòóðû, 1985. – 560 c. Ôèçèêà êîñìîñà. Ìàëåíüêàÿ ýíöèêëîïåäèÿ.–Ì.:Ñîâåòñêàÿ Ýíöèêëîïåäèÿ, 1986.– C.364. Reid H.F. The elastic–rebound theory of earthquakes. University of California Publ. Geol. Sci. – 1911. –V. 6. – P. 413–444. Yu.B. Brodsky: THE HYPOTHESIS OF THE RELATIONSHIP BETWEEN THE CURRENT... Page 1 Page 2 Page 3 Page 4 Page 5 Page 6