Last News

30:09:2016

Европейский сейсмологический центр EMSC сообщил, что в центральной части Италии произошло землетрясение магнитудой 6,1. По данным Геологической службы США (USGS), сила толчков составила 6,2.

14:01:2016

Elchin Khalilov has informed about the beginning of new project GNFE under the name "Geodynamic monitoring and hazard early warning system in landslide areas:"GeoDyn".

The new project is based on use of long-term experience effective application of international systems and geodynamical monitoring for forecasting of earthquakes. The project's mission is to create an effective technology for monitoring and early warning of people about the danger of a landslide, reducing thereby the risk to potential victims and other negative consequences of landslides affecting cities and high-risk industrial facilities (main highways and railways, dams, fuel storages and warehouses for toxic substances, petrochemical plants, etc.).

04:12:2015

Prof. Elchin Khalilov is President of the Global Network for the Forecasting of Earthquakes GNFE (UK) and Chairman of GEOCHANGE International Committee (Germany), gave the forecast of seismic activity of the world till 2026 on behalf of the above-mentioned organizations.

30:11:2015

Проф. Эльчин Халилов - Президент Глобальной Сети Прогнозирования Землетрясений GNFE (UK) и  Председатель Международного  Комитета  GEOCHANGE (Germany), представил  прогноз  сейсмической активности  мира до 2026 года от имени вышеуказанных организаций. 

 

Tutorials

CONTENTS

CHAPTER 1

Forecasting of earthquakes:

The reasons for previous failures and the

new philosophy

 

Introduction

1.1.Registration of different harbingers at large distances from epicenters.

1.2.Seismic-gravitational harbingers

1.3.Tideless variations of gravity

1.4.Geochemical harbingers

1.5.Seismic-hydro-geological harbingers

1.6.Seismic harbingers

1.7.Low-frequency three-dimensional variations of gravitational field

1.8.Classification of the considered "long-range" harbingers

1.9.What and how did the seismologists forecast heretofore?

1.10. About the possible influence of tectonic waves on different

properties of the geological  medium

1.10.1.General information

1.10.2. Gravitational harbingers of earthquakes.

1.10.3. Geo-chemical harbingers of earthquakes

1.10.4. Hydro-geological harbingers of earthquakes

1.10.5. Seismic and acoustic harbingers of earthquakes

1.10.6. Electric, magnetic, electromagnetic, optical and

other harbingers of earthquakes

1.10.7. Main reasons for  inefficiency of classical methods

of earthquake forecasting

1.11. Local harbingers of earthquakes

1.12. Long-range harbingers of earthquake

1.13.Fundamental mistake of seismology in short-term

forecasting of earthquakes

1.14.What to do?

References

 

CHAPTER 2

"ATROPATENA" EARTHQUAKE FORECASTING STATIONS

PHYSICAL PRINCIPLES AND THE FIRST RESULTS

FIRST RESULTS

Introduction

2.1. Methodology

2.2. Results

2.3. Conclusions

References

CHAPTER 1

Forecasting of earthquakes: The reasons for failures and the new philosophy

Introduction

Throughout history, people have tried to accurately predict cataclysms. Ancient historical sources, legends, myths, and religious writings all detail their efforts. They used what was accessible to them based on their level of knowledge and philosophy. They tried to use astronomical phenomena and associated the natural cataclysms with them. For example, ancient people took the solar eclipses, approaches of Mars to the Earth, appearance of spots on the Sun, unusual behavior of animals and unusual phenomena in the atmosphere as special signs of approaching catastrophes.

How far have modern scientists come from their predecessors? Modern science studies with great interest the influence of the planets of the solar system, solar activity, and other cosmic factors on seismicity and volcanism. Meanwhile, for short-term forecasting, the different harbingers of earthquakes are used much as they were in earlier times. The main difference is in the explanations of the connections between the observed harbingers and the gestation of the earthquakes. Another significant difference is the application of modern high technology recording equipment. In other respects, the "philosophy" of forecasting the earthquakes hasn't changed that much, practically speaking.

Scientific research aimed at creating technology to forecast earthquakes has been financed for about 100 years in many developed countries of the world. However, the absence of serious achievement caused disappointment amongst public officials and in the wider mass population. Seismologists, who forecast earthquakes and spent millions of dollars, found themselves in difficult and delicate situations. Most of them were looking for justifications of their scientific failures, and gladly found them during an international scientific meeting in London on 7-8 November 1996, on the subject of interrelation of earthquakes with other phenomena in order to forecast them. Transactions of this meeting were published in Geophysical Journal International, vol. 131, pgs 413 to 533, 1997.

During this authoritative forum, the famous seismologist Dr. Robert J. Geller declared the impossibility in principle of forecasting earthquakes. His main idea is that the earthquake source has such a large probability of randomness that it approximates a chaotic process. Many further articles and speeches of Dr. Robert Geller propagate his ideas about the impossibility of forecasting the earthquakes. This idea is reflected in his basic statement: "Research in the sphere of forecasting earthquakes has been carried out for more than 100 years without evident success. The results of research didn't result in great achievements. The extensive research was not able to find reliable harbingers. Our theoretical work supposes that break displacement is a nonlinear process, which is very sensitive to unknown details of structure of the Earth in bulk, and not only in immediate proximity to the epicenter. The reliable accordance of alarms about unavoidable strong earthquakes is inefficient and impossible" /9/.

What did Dr. Robert Geller achieve with his critical statements?

First, he gave "seismologists-pessimists" good reason to "scientifically" avow their failures.

Second, he slowed down the development of science in the sphere of earthquake forecasting for more than ten years, because after his speeches "the epidemic of mass pessimism and skepticism" arose in the sphere of earthquake forecasting.   

Third, he divided seismologists into two enemy camps - the adversaries of earthquake forecasting and the adherents of earthquake forecasting.

The followers of Robert Geller published articles which "proved" the impossibility, in principle, of earthquake forecasting /10, 12-15/.

Robert Geller thinks that "Modern theories of earthquakes consider that they (earthquakes, author's notes) are critical or self-organizing critical phenomena, which means the system, which is kept on the border of chaos with integral random elements and the dynamics of avalanche, has a strong sensitivity to weak variations of stress."

Does Robert Geller really believe that a part of "chaos" in the process of display of all earthquake harbingers increases a part of strict regularity?

The fact of the matter is that a mistake in choosing the physical model causes mistakes in all further mathematical models. Everything depends on the correctness of the choice of "system of coordinates" or "reference frame". If your physical model is inside the system of coordinates where the physical processes are changed together with the system of coordinates, you will never "see" these processes. In order to see these processes, you have to exit this system of coordinates and go to another system of coordinates. This conclusion proceeds from the postulate of special relativity theory. We advise Dr. R. Geller and other critics not to forget this postulate of special relativity theory.

We don't want to say that Dr. Robert Geller and his followers are not at all right. Our assertion is that these statements are true only for one type of earthquake harbinger - local harbingers. But the point of view of Dr. Robert Geller and his followers isn't accurate for long-range earthquake harbingers, which we'll talk about below. Meanwhile, we also want to draw attention to the works with optimistic viewpoints of the problems of earthquake forecasting /17-21/.

Fortunately, in recent years there has been a significant impulse into research on the problem of earthquake forecasting, and this new research results in a better understanding of the physical origin of earthquake harbingers and the reasons for failures in their forecasting.

1.1.Registration of different harbingers at large distances from epicenters.

There are more than 300 known earthquake harbingers of different character and origin.

During recent years, a number of scientists published the research results indicative of the possibility of the registration of harbingers of strong earthquakes at distances of more than 5000 km, and in some cases more than 10,000 km /1-4, 6-7,11, 21-24/.

1.2.Seismic-gravitational harbingers

So, as a result of research carried out by the Department of Physics of the Earth at Petersburg's State University, the Seismic-Gravimetric Complex in Petersburg registered a long-term tensile deformation (vertically) with a duration of 12 days and nights, which foretold the cycle of strong earthquakes of December 2004, including the strongest earthquake on northern Sumatra island on 26.12.2004, which caused a catastrophic tsunami. Before each strong earthquake, deformations of lesser continuation (1-2 days) were registered. Also noted was an increase in intensity of seismic-gravitational fluctuations which accompany these deformations, the beginning of which always preceded the moment of breaks of strong earthquakes by 1-4 days. Initial estimates of speed and length of waves were made. Low-speed waves (speed from 0.35 to 0.68 km/sec) of seismic origin had wave lengths from 1520 to 7310 km. As a result of analysis of the received data, the scientists came to the conclusion that the observed fluctuations are connected with deformational processes which are taking place inside the continent in a complex block-hierarchical structure /3/.

1.3.Tideless variations of gravity

So, since 2002 the Scientific-Research Institute of Forecasting and Studying the Earthquakes (Baku) has carried out the continuous measurement of tideless variations of gravity in the "Binagadi" station, which is located in Absheron Peninsula 24 km from Baku. The measurements were carried out simultaneously by four high-precision quartz gravimeters of types KB and KC /21/.

As a result of measurements and interpretation of the received data, signals in variations of gravity which preceded the strong earthquakes were found, the epicenters of which were at large distances (in the radius of two thousand to tens of thousands of km) from the registered stations. In the process of interpretation of results of research, gravitational effects from lunar and solar tides were deduced. As is known, the solar tides cause variations of gravity which do not exceed 0.1 mGal, and the amplitude of lunar variations is about 0.2 mGal..

Changes of tideless variations of gravity were registered before strong earthquakes in Indonesia, Pakistan, Japan, Taiwan, India, the Philippines, Iran.

Statistic data show that the gravitational signals were registered more than in 85% cases, on the average, 8-15 days before strong earthquakes /21/.

1.4.Geochemical harbingers

In a series of works (A. A. Hasanov, R. A. Keramova, 2006) was noted the change of geochemical composition of fluids on the registering stations of the Republican Centre of Seismologic Service of Azerbaijan, before catastrophic earthquakes (MLH = 8.9) in Indonesia on 26.12.2004 at a distance of about 6000 km from the epicenter of the earthquake /1/. In the works of A. A. Gasanov and R. A. Keramova, changes of hydro-geo-chemical mode in the registering points of Azerbaijan before strong (MLH ≥ 6.0), deep-focus (h ≥ 100 km) earthquakes are considered, the sources of which are within Hindu Kush seismic zone of Alpine-Himalayan tectonic belt of the Earth, in spite of the remoteness of these sources from the objects of observations (∆=2000-5000 km) /1,11/.

1.5.Seismic-hydro-geological harbingers

Studying of seismic-hydro-geological harbingers of earthquakes allowed determination of the presence of a connection of changes of the level of ground waters in the region of Kamchatka Peninsula with strong earthquakes, more than 8000 km from the measurement point /3/.

1.6. Seismic harbingers

A series of works /4,6/ determined that before strong earthquakes, seismic stations situated more than 3000 km from the epicenters displayed synchronization of micro-seismic noise.

The authors of the research (G. A. Sobolev and others, 2007; Lyubushkin, 2008) offer to use this effect as a harbinger for forecasting strong earthquakes. It was determined that at large distances from epicenters of strong earthquakes, seismic stations registered the synchronic fluctuations of micro-seismic noise with durations of 1-3 hours a few days before the tremor.

1.7.Low-frequency three-dimensional variations of gravitational field

During recent years began research of earthquake harbingers, which were based on the 2003 discovery of a previously unknown effect of low-frequency three-dimensional changes of gravitational field before strong earthquakes at large distances from their sources, at times as large as 10,000 km (E. N. Khalilov, 2003) /7, 22, 24/.

These signals are registered with the help of an unusual physical instrument – the "Torsion three-component detector of low-frequency gravitational variations" - which was called the ATROPATENA station by the author. The ATROPATENA station uses a physical principle never applied before. The method of measuring and the instrument itself are patented in PCT, Geneva (E. N. Khalilov, Method for recording the low-frequency gravity waves and device for the measurement thereof. Patent of PCT. WO 2005/003818 A1., Geneva, 13.01.2005) /23/.

The ATROPATENA station continuously registers in three mutually-perpendicular directions the influence of changes of gravitational fields of geological origin on interaction of masses in a "Cavendish balance" and tideless variations of gravity. So, this simultaneously answered one of the most asked questions of fundamental physics about reasons of variations of "gravitational constant", registered by different scientists at different times in many countries of the world.

From 2007 there were officially given many forecasts of strong earthquakes for the Special Region of Indonesia – Yogyakarta, to the Pakistan Academy of Science, and to the Center of Studying the Earthquakes of Pakistan, with which the Scientific Research Institute at Institute of Earthquakes has bilateral memoranda about cooperation.

1.8. Classification of the considered "long-range" harbingers

So, the brief review allowed marking out a few harbingers of earthquakes, which appear at large distances between registering points and epicenters of earthquakes:

  • Seismic-gravitational anomalies /2/;
  • Tideless variations of gravity /21/;
  • Changes of hydro-geo-chemical mode /1,11/;
  • Changes of the level of ground waters /3/;
  • Synchronization of micro-seismic noise /4, 6/.
  • Long-period three-dimensional variations of gravitational field /7/.

We didn't review some other harbingers, which also display themselves at large distances from epicenters of strong earthquakes (variations of different parameters of ionosphere, electromagnetic noise disturbances, electric, magnetic and other harbingers).

 1.9. What and how did the seismologists forecast heretofore?

The philosophy of short-term forecasting of earthquakes has not undergone essential changes during the whole history of its existence. The basis of all technologies of short-term forecasting of earthquakes is to create a network of stations which register the changes of geophysical, geochemical, hydro-geological and other parameters of the geological medium before strong earthquakes near potential sources of possible earthquakes. It is believed that the more the stations and the closer they are to the potential earthquake source, the higher the probability of successful forecasting.

Meanwhile, in practice it is much more complicated. In spite of the increasing of the number of stations in immediate vicinity from potential sources, the probability of authenticity of short-term forecasts hasn't gone over the level of 70-75%.

As was shown in the brief review, changes in the geological medium at large distances from the sources of future earthquakes take place before strong earthquakes. What is the physical mechanism of these changes?

In the works /7/ the authors come to conclusion that the main reason for long-period three-dimensional variations of the gravitational field are tectonic waves, which are generated by the earthquakes source in the process of its gestation.

1.10. About possible influence of tectonic waves on different

properties of the geological medium

1.10.1.General information

Bases of the concept of tectonic waves were laid in the mathematical model of V. Elsasser in accordance with which the redistribution of compressive forces, averaged on cross-section of elastic lithosphere, are compensated with the tangential forces, which arise under horizontal shift of the lithosphere along the viscous asthenosphere (Elsasser W., 1969). Later, this model was used for quantitative assessment of aftershock activity transfer (Kasahara K., 1985; Baranov B.V., 1980).

Afterwards, Elsasser’s model was supplemented by J. Rice with the effect of viscous-elastic reaction of the asthenosphere on horizontal shifts of the lithosphere. He also took into account the real two-dimensionality of the process (Rice J. R., 1982). Theoretical analysis of the propagation of waves of seismic activity in the lithosphere was given in the works of F. Lehner and other researchers (Lehner F. K., Li V. C., Rice J. R., 1981). The effect of bending of the lithosphere on the liquid lithospheric base found its reflection in the works of Nadai A. and Artushkov E. V. (Nadai A., 1969; Artushkov E. V., 1979). Later, in the works of Nikolayevskiy N. V., Karakin A. V. and Lobkovskiy L. I. an attempt was made to develop the two-dimensional theory of waves of bending - compression of the lithosphere on the viscous asthenosphere (Karakin A. V., Lobkovskiy L. I., 1984).

V. V. Rujich put forward a hypothesis (Institute of the Earth's Crust, Irkutsk, oral report, 1998), according to which each earthquake is accompanied by the generation of compressional waves with extremely low velocity of propagation (V<0.1 m/sec). V. V. Rujich gave them the name slow deformation waves (SDW). This hypothesis corresponds well to the contrast deformation anomaly, fixed by Stepanov I. I. on 27 June 1998, 26 days after the Shipun earthquake of 1 June (which consisted of 3 contrast single impulses with amplitudes of 92, 140, and 43 conventional units and intervals between them of about 7 hours). It allows assessment of the propagation velocity of SDW of about 0.05 m/sec. In the high background of cubic strains during the day of perceptible earthquakes 1.5 - 24 hours before the event, unit impulse signals which exceed the noise by a factor of 2-3 or more times are observed. For example, on 1 June 1988 two such signals were registered with amplitudes of 38 conventional units for a day and night and 41 conventional units 1.5 hours before the event. And on 27 August 2000 before a weaker event two impulse signals were also noted: 68 conventional units 6.5 hours and 40 units 3.5 hours before the earthquake at a background of about 20 units. It allows one to suppose that such impulse signals in the high background can take the role of short-term harbingers before strong seismic events.

More extensive analysis of research devoted to tectonic waves with a large number of references to original sources has been cited in the works /7,24/.

In what way can the tectonic waves have an influence on changes of different parameters of the natural environment? 

1.10.2. Gravitational harbingers of earthquakes.

Fig. 1.1 schematically shows the model of tectonic wave generation by the earthquake source and their successive passage under the ATROPATENA-AZ (Azerbaijan) and ATROPATENA-PK (Pakistan) stations.

Fig.1.1. Schematic model of tectonic wave generation by the earthquake source.

In accordance with many research efforts and the rated models of different authors, the tectonic wave, similar to the seismic wave, has compressional and transverse components. Fig. 1.1 shows the model of a possible mechanism of non-spherical tectonic wave propagation by an earthquake source.

The compressional tectonic wave propagation causes alternating changes of rock density in a large stratum of the lithosphere, along the direction of wave movement, Fig. 1.2. Successive compression and expansion of the lithosphere in the field of the passing condensational wave causes an alternating increase and decrease of the mass of the rocks under the registering stations. Therefore, the ATROPATENA stations register the alternating changes of gravity acceleration, as is shown in the model, Fig. 1.2.

Fig.1.2. Model of influence of compressional tectonic wave on alternate changes of rock density and the corresponding variations of gravity.

1-5 - the registering stations ATROPATENA.

Movement of transverse tectonic waves causes alternating changes of rock density in a large stratum of the lithosphere, perpendicular to the direction of wave propagation, Fig. 1.3. The successive alternate compression and expansion of lithosphere in the field of the passing transverse wave, causes an alternating increase and decrease of the mass of the rocks from different sides from the registering stations. Therefore, the ATROPATENA stations register the alternating changes of the gravitational field in two perpendicular horizontal directions, as is shown in the model, Fig. 1.3.

Fig.1.3. Model of influence of the transverse tectonic wave on variations of changes of the density of rocks in horizontal direction.

Fig. 1.4 shows an example gravitogram which was recorded by the ATROPATENA-AZ station of earthquake forecasting before strong earthquakes in the province of Sichuan (China) in May 2008.

Fig. 1.4. The registered anomalies of the gravitational field by the ATROPATENA-AZ (Baku) station before strong earthquakes in the province of Sichuan, China in May 2008.

Thereby, the physical mechanism of influence of tectonic waves on the gravitational field of the Earth, to our opinion, is logically and convincingly substantiated. This mechanism can explain all existing harbingers of earthquakes of gravitational character: long-period three-dimensional variations of gravitational field, tideless variations of gravity, seismic-gravitational effects, variations of gravitational gradient, etc.

Meanwhile, there is also a logical explanation of the mechanism of influence of tectonic waves on geochemical characteristics of the geological medium, including hydro-geochemical, gas-geo-chemical ones, and others.

 1.10.3. Geo-chemical harbingers of earthquakes

The work of I. I. Stepanov (I. I. Stepanov, 2002) gives very important, in our opinion, results of research on monitoring of volume deformations with the help of the geochemical deformometer in the region of Avachin bay /5/. The concept, taken as the principle of the deformometer, is based on I. I. Stepanov’s discovery that the special condition of atoms of some chemically inert elements in the volume of crystal lattices of minerals is similar in some relations to the ideal gas, and therefore, they are called "quasi-gaseous". In I. I. Stepanov’s opinion, such substances are able to play the role of a sensitive indicator of the quantity of deformations of minerals’ crystal lattices. When the volume of the lattice decreases, the partial pressure of this "quasi-gas" inside it increases. So far as this process in first approximation can be considered adiabatic, some of the atoms gain additional energy and the possibility to overcome the potential barrier which exists on the borders of the partition / lattice / open environment. If the mineral system’s surrounding atmosphere is a closed loop, then the equilibrium position inside it will vary to increase the concentration of steams of this substance in the gas over the mineral. This state is reversible, and when the volume of crystal lattice of the mineral increases, the atoms "extruded" from it come back to the mineral. So, by continuously measuring the content of atoms of this element in the gas over the mineral, one may judge of degree of mineral deformation. With a sufficiently low detection limit of the measuring device, registration of small deformations, about 10-6 or less, becomes possible.

Thereby, the method applied by I. I. Stepanov /5/, measuring the volume of deformations of the geological medium with the help of the geochemical deformometer, uses a principle which can be also displayed in natural geological medium during the passage of tectonic waves.

As is known, rocks and minerals have structural anisotropy, and consequently, they are compressed differently depending on the direction of compression. Under this feature, the peculiar selectivity of geochemical indicators of the medium (liquid or gaseous) is observed, depending on the direction, when a tectonic wave passes through the rocks.

Similarly, changes in radon concentration in zones of deep breaks can occur under the influence of a passing tectonic wave.

1.10.4. Hydro-geological harbingers of earthquakes

Changes in the level of underground waters during passing of tectonic wave are also logically explained by the process of extrusion of water at compression of pores of rocks (increasing the level of groundwater) and the drawing of water into the pores at increasing of their volume under influence of tensile strains (decreasing of level of groundwater).

1.10.5. Seismic and acoustic harbingers of earthquakes

As is known, the seismic characteristics of a medium directly depend on its density, particularly, the velocity of seismic wave propagation, the refraction index and absorption coefficient, spectral characteristics, etc.

Therefore, the alternating changing density of large rock masses under the influence of a passing tectonic wave causes periodic changes of its seismic properties that cause modulation of micro-seismic noise and the so-called "synchronization of micro-seismic noise" by the tectonic wave.

 Anisotropy of rocks put down in layers of the lithosphere causes the tectonic waves which pass at different angles to seismic stations, to synchronize (modulate) the micro-seismic noise differently. This means that there is selectivity on the direction (asymmetry of directional diagram) of kinematic and dynamic parameters of micro-seismic noise modulated under the influence of tectonic waves /25/.

Similarly substantiated is the display of acoustic, particularly ultrasound and infrasound, harbingers of earthquakes.

 1.10.6. Electric, magnetic, electromagnetic, optical and other harbingers of earthquakes

Alternating changing stress conditions of the geological medium under influence of a tectonic wave should cause visibility of other known harbingers of earthquakes too. As is known, the change of the level of underground water and density of rocks causes changes in electric properties of rocks that displays as electric harbingers of earthquakes (changes of electrical resistance of rocks).

Also, changes in the density of rocks causes changes in their magnetic properties (changes of density and other characteristics of magnetic field).

In addition, under the influence of alternating deformations, quartz-containing rocks (piezocrystals) can display the piezoelectric effect and, as a consequence, indicate the appearance of static electricity in huge stratum. It, in its turn, can influence the ionization of the lower layer of atmosphere above the projection of the front of a tectonic wave on the surface of the Earth.

1.10.7. Main reasons for inefficiency of classical methods of earthquake forecasting

The results of our research and discussions have shown that the display of earthquake harbingers has a considerably more complicated nature than seismologists have previously thought /7/.

Thereby, we can suppose that there are two types of earthquake harbingers:

- Local harbingers of earthquakes;

- Long-range harbingers of earthquakes;

The biggest problem is that the main causes of both types of earthquake harbingers are the same mechanisms - changes of the stress condition of rocks.

1.11. Local harbingers of earthquakes

Local harbingers of earthquakes are directly connected to the processes of critical increases of stress conditions of rocks in the focal zone. As a result, the processes of compression, extension, displacement, bend, etc. of large strata of the Earth in different areas of focal zone are displayed. It is practically impossible to model this process because of its nonlinearity /Dr. Robert J. Geller, 1997/. Therefore, the same source of an earthquake can have different (dissimilar) displays of harbingers during repeated earthquakes. The majority of local harbingers of earthquake display unstably near the earthquake epicenter (gravitational, seismic, geo-chemical, electrical, magnetic, electromagnetic, deformational ones, etc.).

1.12. Long-range harbingers of earthquake

Long-range harbingers of earthquakes are secondary harbingers and reflect changes in different parameters of geological medium (gravitational, seismic, geo-chemical, electrical, magnetic, electromagnetic, deformational parameters, etc.) under the influence of tectonic waves, generated by sources of upcoming earthquakes. The physical mechanism of the display of these harbingers was described above.

1.13.Fundamental mistake of seismology in short-term forecasting of earthquakes

From the above-mentioned arguments it is clear that in short-term forecasting of earthquakes, local and long-range harbingers of earthquakes are registered simultaneously. Therefore, frequently, as a principle component of local short-term forecasting of earthquakes (in the radius of several hundreds of kilometers from the epicenter of the earthquake) were taken long-range harbingers from earthquake sources which are large distances from the registering points (up to 10 000 kilometers).

As the local harbingers obey the model of Doctor Robert Geller, their display is hardly useful for forecasting.

Meanwhile, the long-range harbingers of earthquakes, which are the result of generation of tectonic waves by the sources of strong earthquakes, are stable and high-quality. As the experience of using the ATROPATENA station during two years shows, the long-range gravitational harbingers of earthquakes allow forecasting with 90% accuracy, and this probability will increase as new ATROPATENA stations are included into the Global Network for the Forecasting of Earthquakes (GNFE).

1.14. What to do?

During almost 100 years of history of forecasting earthquakes, seismology has not only stored extensive information about different harbingers of earthquakes, but also created unique local networks of points monitoring different parameters of the geological medium around focal zones of strong earthquakes and deep breaks. Multiple seismological polygons for monitoring of the geological medium were created in different countries.

In our opinion, the only way out of the situation that has arisen is the creation of the Global Network for the Forecasting of Earthquakes (GNFE), consisting of stations for forecasting earthquakes united into a single network, registering the most stable and high-quality long-range harbingers of earthquakes. The global network must be connected with multiple local networks. Thereby, the Global Network for the Forecasting of Earthquakes will allow registration of long-range harbingers of earthquakes, and the local networks will simultaneously register the local harbingers. Interconnecting of long-range and local harbingers will increase the accuracy of short-term earthquake forecasting.

The beginning of a network has been created on the basis of the ATROPATENA stations with points in Baku (Azerbaijan), Islamabad (Pakistan) and Yogyakarta (Indonesia).

References

  1. A. A. Hasanov, R. A. Keramova. Reflection of global geodynamical processes in seismic-geo-chemical mode of fluids of Azerbaijan at the example of catastrophic earthquake in the Indian ocean (26.12.04; MLH =8.9). In the book Geophysics of XXI century: 2005, M. collected papers of GEON. "Scientific world". 2006, pp. 326-330.
  2. L. N. Petrova, E.G. Orlov, V. V. Karpinskiy. large-scale deformations of the Earth before strong earthquakes on the observations with the help of seismic-gravimeters. Physical bases of forecasting the rock failure. Thesis of reports of VII International school-seminar. Geophysical observatory "Borok", 17-21 October 2005. M., 2005, p. 46.
  3. G. N. Kopilova, T. K. Pinegina, N. N. Smolina, Seismic-hydro-geological effects of the strongest earthquakes (at the example of Kamchatka region), pp. 166-173. Collected materials of scientific meeting "Problems of modern seismic geology and geodynamics of Central and Eastern Asia (2 volumes). 18-24 September 2007 IZK SO RAS Irkutsk.
  4. A. A. Lyubushin. Micro-seismic noise in a minute's diapason of periods: properties and possible forecasting features. Physics of the Earth. #4, April of 2008, pp. 17-34.
  5. I. I. Stepanov. Monitoring of cubic strains with the help of geochemical deformometer in the region of Avachin bay. In the collection Modern volcanism and the processes connected with it. Materials of the anniversary session of Kamchatka scientific center of DVO RAS, devoted to 40 -year of Institute of volcanology, 8-11 October 2002.
  6. G. A. Sobolev, A. A. Lyubushin, N. A. Zakrjevskaya. Asymmetric impulses, periodicity and synchronization of low-frequency microseisms. Volcanology and seismology. #2, March, April of 2008, pp. 135-152.
  7. V. Y. Khain, E. N. Khalilov. Space-time regularities of seismic and volcanic activities. Bulgaria, Burgas, SWB, 2008, p. 304.
  8. Aki K., Earthquake, prediction, societal implications, Univ. Southern California, From Reviews of Geophysics.http://www.agu.org/revgeophys/aki00/aki00.html
  9. Dr. Robert Geller. Nature, vol. 385, pg 19-20, 1997
  10. Robert J. Geller, D. D. Jackson, Y. Y. Kagan, F. Mulargia, Earthquakes cannot be predicted, From Science.
    http://scec.ess.ucla.edu/%7Eykagan/perspective.html.
  11. A. G. Gasanov, R.A.Keramova - Hydro-geo-chemical criteria of Caspian earthquake (25.11.2000) in ground waters of north-east and north-west of Azerbaijan. International Conference Natural Hazards: mitigation and management. March 12-15, 2001, India, Amritsar.
  12. Ian Main, Is the reliable prediction of individual earthquakes a realistic scientific goal?, Debate in Nature, 1999
    http://www.nature.com/nature/debates/earthquake/equake_contents.html
  13. Ian Main. Earthquake prediction: concluding remarks. Nature debates, Week 7, (1999).
  14. Ludwin R. S., 2001, Earthquake Prediction, Washington Geology, Vol. 28, No. 3, May 2001, p. 27.
  15. Predicting and earthquake.http://earthquake.usgs.gov/hazards/prediction.html
  16. Robert J. Geller, D. D. Jackson, Kagan Y. Y., Mulargia F., Earthquakes cannot be predicted, From Science.
    http://scec.ess.ucla.edu/%7Eykagan/perspective.html
  17. Max Wyss, Not yet, but eventually, Nature debates, Week 1, (1999).
  18. Thanassoulas, C., and Klentos, V., (2001). Very short-term (+/- 1 day, +/- 1 hour) time prediction of a large imminent earthquake. The "second paper", Institute of Geology and Mineral Exploration (IGME), Athens, Greece, Open File Report A. 4382, pp. 1-24.
  19. Mavrodiyev Cht., The electromagnetic fields under, on and over Earth surface as "when, where and how" earthquake precursor, European Geophysical Society, Geophysical Research Abstracts, Vol. 5, 04049, 2003.
  20. Mavrodiyev S. Cht. Applied Ecology of the Black Sea, ISBN 1-56072-613-X, 207 Pages, Nova Science Publishers, Inc., Commack, New York 11725, 1998.
  21. Khain V. Y., Khalilov E. N. Tideless variations of gravity before strong distant earthquakes. Science Without Borders. Volume 2. 2006/2006. ICSD/IAS H&E, Innsbruck, 2006, pp. 319-339.
  22. Khalilov E. N. About possibility of creation of international global system of forecasting the earthquakes "ATROPATENA" (Baku-Yogyakarta-Islamabad). Natural cataclysms and global problems of the modern civilization. Special edition of Transaction of the International Academy of Science. H&E. ICSD/IAS H&E, Innsbruck, 2007, pp. 51-69.
  23. Khalilov E. N. Method for recording the low-frequency gravity waves and device for the measurement thereof. Patent of PCT. WO 2005/003818 A1., Geneva, 13.01.2005).

 

CHAPTER 2

"ATROPATENA" EARTHQUAKE FORECASTING STATIONS:
PHYSICAL PRINCIPLES AND THE FIRST RESULTS

Introduction

As the accuracy of measuring the gravitational constant G increased over time, the differences between the results of measurements of G made by different scientists increased in a strange manner.

First, P. Dirac published the possibility of changes in the gravitational constant (1). Afterwards, a great number of different scientists’ researches were devoted to this problem.

P. Dikke showed the theoretical possibility of G decreasing with the increasing age of the Universe (2). In the opinion of K. Stanukovich, G increases with the age of the Universe (3).

Izmailov, Karagioz, and Parkhomov (4) have received variations in the measured values G which considerably increased the error of the measuring instrument.

Meanwhile, summing up their researches, the above-mentioned scientists came to the following conclusion: "The analysis of variations of the results of measurements of the gravitational constant shows that the changes of geomagnetic field, the instability of temperature and atmosphere pressure, the residual gas flows in the vacuum camera, the changes of plant tilt cannot cause the observable effects. Variations of gravitational field connected with the changes of relative position of the Earth, the Moon and the Sun are too small for direct sensible influence on the results of measurements."

The results of research of variations in G were published in World Data Center (http:zeus.wdcb.ru/wdcb/sep/GravConst/welcome.html). In (5), it is shown that variations of the gravitational constant have a certain cyclicity. In (6), the possible influence of super-long gravitational waves on indicators of a Cavendish balance is referred to. Morganstern R. made an assumption about the existence of a cosmological limit in the possible variations of G (7).

To date, the two most accurate measurements of G have been made by groups of scientists at the University of Washington in Seattle and the International Bureau of Weights and Measures in Paris. In both cases the error margin of the experiments were 1/10000; however, the difference of the received values is considerably more than the probable errors. In Seattle research resulted in the value (8):

G=(6.674215±0.000092) · 10-11 m3 · kg-1 · s-2.

Jean-Paul Mbelek and Marc Lachieze-Ray from the French Commission on Atomic Energy declared that they had succeeded in understanding the reason for similar discrepancies between experimental values. The researchers supposed interference of gravitational and electromagnetic fields is at the heart of the observed discrepancies.

In their work, they produced the calculations of the expected values of the gravitational constant in different regions of the planet. Into the basis of the calculations were put theories supposing the availability of latent dimensions in space, in particular, string theory, in the frameworks of which the electromagnetic and gravitational fields are combined (9).

In the calculations, it turns out that terrestrial gravity will be stronger in places where the magnetic field is stronger; that is, the maximum values can be expected in the regions of north and south magnetic poles. In their opinion, the available experimental data fully agree with the theory; however, the carrying out of precision measurements both in the regions of the poles themselves and in equatorial regions is required.

Meanwhile, some scientists do not share this concept (10).

In (11), it is noted that during the last few years the spread in measured values of the gravitational constant has reached 0.7%. A new experiment of a group of Swiss physicists from Zurich University received a result which is different from the French result. So, in a special cemented cellar near Willigen (Switzerland), they measured by means of a sensitive laboratory balance, the difference in the mass of two small weights, under or above which were placed two large vessels of mercury with the weight of 13 tons. Measuring the changes of weights of trial masses by the ultra-sensitive balance, the researchers calculated the value of gravitational constant to be:

G = (6,6754 ± 0,0005) · 10-11 m3 · kg-1 · s-2

Their data are different from the results of the group in Seattle and of the French scientists.

In any case, attempts to specify the measured values of G so far cause strengthening of differences in the results received by different scientists around the world. It accentuates some confusion on the part of the scientists, as the variations of G do not agree with the basic rules of general relativity.

It could be possible to speak about mistakes related to the error of measurements or unaccounted disturbances, if they were single instances. However, the changes in time and space in the measured values of G observed by many scientists during last ten years are increasing proportionally to the rising accuracy of the measuring systems.

Modern ideas of gravity were for the first time described by A. Einstein within general relativity (17). In accordance with general relativity, the coefficient G is constant.

2.1. Methodology

A new instrument for experimental study of the space-time variations of measured values of G was created, called the ATROPATENA detector (PCT patent pending) by the authors (12).

ATROPATENA is a system of sensors closed and isolated from the environment, using the physical principle of the Cavendish balance, with small weights on the ends of two (instead of one) mutually perpendicular balance-beams hung by threads 2. Between the small weights large weights are placed equally spaced 3, Fig. 2.1 (a).

The third measuring sensor, the trial mass 4, is hung on a special elastic lever and makes available the possibility of vertical displacements during changes in the relative values of acceleration of gravity, Δg. Variations of Δg are stipulated for lunisolar floods and for the appearance of local gravitational anomalies, which can be caused by the changing of density of rock mass under the instrument as a result of changes in their stress condition, and consequently their mass.

As seen in the scheme, on the balance-beams with the weights 2 and on the lever of the vertical sensor 4, there are tiny mirrors on which three laser beams are directed. Being reflected from the mirrors, the beams hit the sensitive optical matrix 6 and 7, where the transformation of optical signal from laser mark into electric signals and their transmission into an analog-to-digital converter occurs. After that, the digital signal is transmitted to a special block of the computer as the next record in a special format. The software, written at the Scientific-Research Institute of Prognosis and Studying of Earthquakes (SRIPSE), automatically records the information in the form of separate files for a period of time determined by the operator.

In Fig. 2.1 (a) the ATROPATENA instrument is shown schematically.

 

a)                                                                             b)

Fig.2.1. The scheme of the construction (a) and the photo (b) of detector ATROPATENA.
1 – glass body of the detector; 2 – balance-beams with small weights on the ends; 3 – big weights; 4 – trial weight, which is hung on elastic lever; 5 – laser emitters, 6 – sensitive optical matrix for horizontal sensors, 7 – sensitive optical matrix for vertical sensor.

The entire sensitive system is placed into the special, isolated from the environment, glass body 1, where a deep vacuum has been created and is constantly supported (10-4 MPa).

Temperature sensors accurate to 0.1C° are placed in different sections of the sensitive system and connected to the temperature control block. The room where ATROPATENA is located is kept to a consistent temperature with inaccuracy ± 10 C.

For excluding the mechanical effects and for better heat insulation, the vacuum body with the sensitive system is placed into translucent plastic body which also allows for visually observing the work of the system (Fig. 2.1(b)).

Together with the noted sensors, ATROPATENA is also provided with a digital seismic station using a three-component seismic receiver, the information of which is also transmitted to the computer and is continuously digitally recorded in three channels X, Y, and Z.

The registration of seismic fluctuations is necessary in order to exclude the possible influence of these fluctuations on destabilization of the sensitive system of the ATROPATENA detector and the appearance of false anomalies caused by seismic processes.

The remote control of the detector and remote pickup of information minimize the external influences on sensitive system..

All elements of the sensitive system have been made of non-metallic materials to exclude the influence of magnetic fields and electromagnetic radiation on these elements. ATROPATENA is placed in the building of Scientific Research Institute of Prognosis and Studying of Earthquakes in Baku (Azerbaijan). Since 1 April 2007 the station has been in operation, and has recorded high-quality information about variations of gravitational field over time in three axes X, Y, and Z, and the seismologic information simultaneously recorded by means of the Tethys-SD wide-band digital seismic station. First, ATROPATENA was provided for experimental research on the possible influence of super-long gravitational waves on the indications of a Cavendish balance.

If one proceeds from classical ideas of fundamental physics, then the ATROPATENA detector, at first sight, is accepted as an absolutely senseless instrument, as it is considered incontestable that the gravitational constant is a fundamental constant and cannot be changed in time or in space. But the author didn’t rule out the possibility of an influence of super-long gravitational waves on a Cavendish balance and wanted to check out that idea (10).

Meanwhile, ATROPATENA registered numerous signals which have definite regularities and high correlation with strong earthquakes in different regions of Eastern Hemisphere of the Earth. Fig. 2.2 shows the schematic sketch of the actual orientation of Cavendish balance in the ATROPATENA station. The sketch represents the view from above, X and Y designate correspondingly oriented balance-beams with small weights on the ends, and m1 and m2 are large weights. N, S, W, E designate accordingly north, south, west, east.


Fig.2.2. Schematic sketch of actual orientation of Cavendish balance in the ATROPATENA station.

For convenience, we call the recordings of the ATROPATENA detector "gravitograms", by analogy with seismograms. The detailed study of gravitograms with anomalous deflections of measured values of G can explain subtler physical nuances of these processes.

On the gravitograms, the graph Gx reflects the movement of the balance-beam X, and the graph GY reflects the movement of the balance-beam Y (Fig. 2.2), the graph GZ reflects the changes of gravity, that is, the vertical movements of the trial weight. An increase of values GX and GY means approaching of small weights on the balance-beams to the large weights, and a decrease means moving away from the large weights. On the coordinate axis are shown the conventional units, which reflect the deviation amplitude of small weights on the ends of balance-beams relative to large weights.

The registration of values of all three sensors is carried out with discontinuity in one second. Using of red lasers with the length of wave 645 nm and special optical matrixes for registration of the laser mark and its displacements allowed registering the deviations of laser-beams on the angle to 0.1 degree. The whole process of registration takes place in digital form automatically, without participation of the operator, and the received time series are archived by means of a special program.

These deviations correspond with variations of gravitational constant G in the third and fourth digits after the decimal point.

2.2. Results

In Fig.2.3. shows the gravitograms with two gravitational anomalies, registered on 5 January and 10 January 2008.

In both graphs, GX and GY show the conventional units of amplitudes of variations in time of the indications of Cavendish balance, oriented, correspondingly, in parallel with axes X and Y. The axis GZ shows the conventional units of the amplitudes of variations in time of gravity, Δg.


Fig.2.3. Gravitograms of 05 and 10 January 2008.
T – time.

As is seen in the gravitogram of 5 January, whereas small weights of the balance-beam X are moving away from the large weights (GX is decreasing), the weights of the balance-beams and GY are approaching with noticeably more amplitude (GY is increasing). At the same time, GZ also shows the increasing of gravity almost synchronously with GY. The 64 minute lag of the beginning of changes in GZ and GX relative to GY is also notable. Also, GZ comes back to its former position 30 minutes later than GY, whereas GX does it 2.5 hours later than GY. We see that all three sensors show a strongly pronounced gravitational signal, which evidently has the same nature, but with great displacements in time of its registration. The duration of the signal is also quite long at 8 hours. During these anomalies, the seismic station didn’t register any seismic fluctuations which exceed the background noise. In addition, seismic signals cannot have the period of several hours. A strong earthquake took place on 7 January in the region of Indonesia of M(magnitude) 5.9 (coordinates are 0.795 S 134.012 E).

The other example of registration of a quite intensive variation in time of gravitational constant G with strict selectivity to the direction is interesting. This signal was registered only by the sensor GY. The other two sensors, as is seen in the gravitogram, "keep silent". The duration of the signal is three hours. During the recording of the signal, no seismic fluctuations were registered. A strong earthquake of M6.5 took place on 15 January in the region of the Fuji islands (coordinates are 21.966 S 179.530W).

The authors took all data about earthquakes in this article from the catalogues of U.S. Geological Survey Earthquake Hazards Program – USGS http://earthquake.usgs.gov/eqcenter/eqarchives/significant/)


Fig.2.4. Gravitograms of 16 and 20 January 2008.
T – time.

First we’ll consider the gravitogram of 16 January, Fig. 2.4. Because of the absence of signals in GZ, this graph isn’t demonstrated. Since 10:00 the decreasing of value GX and increasing of GY have begun synchronically. As it is seen there is some difference in the form of graphs GX and GY, but the whole tendency shows a high negative correlation, which does not raise doubts. The graphs practically mirror each other. While the small weights of the balance-beam X move away from large weights, the weights on the ends of the balance-beam Y approach, and the same takes place in reverse direction. The duration of the observed signal is 14 hours. A quite interesting signal was also registered on 20 January, when the graphs GX and GY during 2 hours register the signal almost mirrored in both gravitograms. Meanwhile, approximately an hour later, after the appearance of this signal, GZ began to continuously register a high-frequency quasiharmonic signal with the period of 4-8 minutes. After the sensors GX and GY stop registering the signals, GZ continues registering the high-frequency signal right up to 23 January inclusive, and such duration of uninterrupted appearance of that signal is quite unusual for the sensor GZ. On 22 January a strong earthquake of M6.2 took place in Indonesia (coordinates are 1.011 N 97.438 E).

In the gravitograms of 02-03 February, very interesting anomalies were registered, Fig. 2.5. GY registered three alternate long-period signals in series, with periods accordingly 11, 8, and 7 hours, then GX registered the mirror image of these signals, but the first (I) and second (II) of them are modulated by high-frequency constituent with the period of 4-9 minutes, and the modulatory high-frequency signal in both cases lasts about 5 hours.

On 04-05 February on the gravitogram, again the typical signal appears, reminiscent in character the signal of 02-03 February, but the gravitational signal GX is modulated by high-frequency constituent with period of 4-9 minutes at the beginning (III) and at the end (IV) of the anomaly. The duration of the modulatory signal is approximately the same and it is about 2 hours. This fact is quite interesting, as the signal GX is clearly limited at the beginning and at the end of the high-frequency constituent.


Fig.2.5. Gravitograms of 02-03 and 04-05 February 2008.
T – time.

A strong earthquake of M7.2 took place on 8 February (coordinates are 10.725 N; 41.898 W) in the region of the north middle-oceanic ridge in central part of the Atlantic ocean, and on 10 February a strong earthquake of M6.5 took place in the sphere of the south Sandwich islands (coordinates are 60.757 S; 25.582 W). In our opinion, it is possible that the anomalies registered on 02-03 February are connected with the earthquake of 8 February, and the anomalies of 04-05 February are connected with the earthquake of 10 February.

Two strong earthquakes took place on 07 May 2008 near the coast of Honshu in Japan: the first one - at 16:02:01 of M6.2 (coordinates are 36.21S 141.47E) and the second one – at 16:45:20 of M6.8 (coordinates are 36.14S 141.45E). The analysis of the recordings of ATROPATENA showed that on 2 May the sensor GX began to register the intensive negative anomaly “A” (Fig.2.6) which lasted till 3 May 04:25. 2 hours later after this anomaly the sensor GX registered the second negative anomaly “B”, which lasted till 5 May. It is notable that these anomalies are the high-frequency pulse bursts with the periods 3,5 – 6,5 minutes. Two strong earthquakes took place in Japan on 7 May 2008 with a small difference in time. So, the earthquakes took place 5 days after the beginning of recording the anomaly and two days after the anomaly has stopped.

The catastrophic earthquake took place on 12 May 2008 in China in the region of Sichuan at 06:28:00 of M8 (coordinates are 31.08S 103.27E) and the second earthquake took place at 06:43:14 of M6,3 (coordinates are 31.25S 103.68E), as a result of which, according to provisional data, about 70 thousand people died, and the death-roll is being specified now.


Fig. 2.6. Gravitogram of 1-17 May 2008.
A,B,C,D,E,K – the registered anomalies of gravitational field;
1;2 – the earthquakes in Japan near the coast of Honshu on 7 May 2008 of M6.2 (time – 16:02:01) and of M6.8 (time – 16:45:20);
3;4;5;6 – the earthquakes in China, Sichuan on 12 May 2008 of M8 (time – 06:28:00); of M6.3 (time – 06:43:14); Sichuan on 13 May 2008 of M5,9 (time – 07:07:09); Sichuan on 17 May 2008 of M6,0 (time – 17:08:25).

On 9 May two sensors GX and GY simultaneously began to register strong anomalies C, D, E, and K of the gravitational field (Fig. 2.6). GY registered an intense positive anomaly which consists of high-frequency pulse burst with periods of 3.5-8 minutes, and GX registered a negative anomaly which consists of pulse bursts with analogous periods. The amplitude of anomalies of the GY sensor is more than three times larger than the amplitude of anomalies of the GX sensor. The anomalies of GY during visual analysis consist of four well-separable pulse bursts (anomalies) according to amplitude modulation – C, D, E, K. Anomaly K differs from the anomalies C, D, and E, in several respects. First, after completion of anomaly E, GX decreases by two conventional units for 15 hours without modulation, and after returning to the background value, anomaly K begins. Anomaly K begins at 15:22 on 12 May and completes at 09:30 on 13 May. Second, on GY the K anomaly also differs from previous anomalies. Anomaly K begins on 12 May and completes at 10:55 on 13 May, and the lower extent of the values of anomaly K are approximately two units higher than the lower extent of anomalies C, D, and E. After the completion of anomaly K, the values return to the background level.

So, in our opinion, the anomalies C and D are the harbingers of the Chinese earthquakes 3 and 4 (Fig. 2.6), and anomalies E and K are the harbingers of the earthquakes 5 and 6

The ATROPATENA detector has simultaneously registered different variations of G in two mutually perpendicular directions and variations in Δg before distant earthquakes since April 2007 until now in 93% of cases.

In previous research, the author together with V. E. Khain discovered the changes of gravity before distant earthquakes by means of standard gravimeters (13).

Starting from the rules of general relativity, gravitational interaction by its nature represents the changes of space curvature caused by masses and is an integral property.

In the Cavendish balance, the interaction of small weights on the ends of the balance-beams hung on a thin thread with stationary large weights takes place, which causes the turning of balance-beams on their axis for some angle. The angle of the turning of the balance-beam is compensated by the elastic force of torsion of the thread, upon the value of which the gravitational constant is calculated. But if other large weights appear near the Cavendish balance, they introduce additional distortions into the curvature of space formed by the large weights in the Cavendish balance. So, we’d have a new system of weights interacting, where the changes of space curvature will be the resultant one of interaction of weights in Cavendish balance and additional weight. In this case, Cavendish balance would show another result.

In real conditions of the Earth, there are many geological factors which create quite intensive gravitational anomalies, changing in space and in time, that are many times larger than the gravitational effects caused by movement of planets of solar system, including the additive effect of lunisolar floods. These effects can be caused by convective flows in the mantle, movement of lithospheric plates, tectonic waves, etc.

In our opinion, this explains the fact that during last ten years, in spite of increasing accuracy of instruments which register the gravitational constant G up to the sixth digit after the decimal point, it has nevertheless been impossible to register G with accuracy higher the third digit after the decimal point, about which the yearly published data of CODATA witness.

In our opinion, it isn't excluded that ATROPATENA registered tectonic waves which can be emitted by the centers of future earthquakes. Tectonic waves, in contrast to seismic waves, are very slow and long, and are also called "stress waves" (14). Tectonic waves are mechanical (15), as are seismic waves, and in a solid medium they have longitudinal and transversal constituents. Passing through under the station, these waves compress and stretch the thick layers of the Earth and with that they change their density and, as a consequence, their mass. The changing of mass under the ATROPATENA detector is registered by three sensors - X, Y, and Z, depending on the type of wave and its direction. Longitudinal and transverse tectonic waves influence the Cavendish balance differently, depending on the orientation of balance with respect to the wave.

For more accurate determination of coordinates of future strong earthquake, it is necessary to use, at the minimum, three ATROPATENA stations, spread large distances from one another.

2.3. Conclusions

On basis of these researches the author came to several important conclusions:

  1. The anomalous changes of the measured values of gravitational constant G over time have been registered authentically, and they differ from each other depending on the orientation of Cavendish balance.
  2. It has been determined that the variations of the measured values of G, registered by different scientists earlier, are connected, mainly, with the influence of external gravitational fields of geological origin on indicators of the Cavendish balance.
  3. A new instrument has been created, the ATROPATENA detector, which allows continuous registration of changes in time of variations of G in different directions together with the variations of acceleration of gravity, Δg, that gives the opportunity to access to a new resource of physical information about geological and cosmic processes.
  4. The ATROPATENA detector simultaneously has registered time variations of gravitational constant G, which are different in sign and amplitude, in two mutually perpendicular directions and variations of gravity, Δg, before distant earthquakes in 93% of cases, which gives us grounds for creation of a new technology of prognosis of strong earthquakes.

References

  1. Dirac. P.A.M. The cosmological constants. Nature, 139, 323  (1937).
  2. Dicce R., Gravitation and relativity, Moscow, Mir, 251-294  (1965). 
  3. Stanukovich K.P., To a question on possible change of a gravitational constant. DAS USSR, Vol. 147, N 6, 1348-1351 (1962) 
  4. Izmailov V.P., Karagioz O.V., Parkhomov A.G., Researches of variations of results of measurements of a gravitational constant.  Physical though of Russia. N ½, 20-26 (1999).
  5. Izmailov V.P., Karagioz O.V., Measurement of a gravitational constant of torsion balance. Measuring technics. Research of variations of results of measurements of a gravitational constant. Moscow, № 10, 3-9 (1996).  
  6. Khain V.Y., Khalilov E.N.  Rhythms  of  natural  cataclysms  and  super-long  gravitational  waves.  Natural Cataclysms  and  global  problems of the  modern civilization.   Special Edition of Transaction of the International Academy of Science. H&E. ICSD/IAS, Innsbruck, 105-118 (2007).
  7. Morganstern R. Cosmological  Upper  Limit  on  Time  Variation of G.  "Nature", v.232, 109 (1971).
  8. Jens H. Gundlach, Stephen M. Merkowitz. Measurement of Newton's Constant Using a Torsion Balance  with Angular Acceleration Feedback   Phys. Rev. Lett. 85, 2869 - 2872 (2000).
  9. J. P. Mbelek et M. Lachièze-Rey, Possible evidence from laboratory measurements for a latitude and longitude dependence of G, Gravitation and Cosmologyб  8, 331 (2002).
  10. Khalilov E.N. About possible reason of variations of gravitational constant.  Science without borders, Vol.1,  ICSD/IAS H&E. Innsbruck, 227-243 (2004).
  11. Schlamminger S, Holzschuh E, Kundig W. Precision Electromagnetic Measurements Digest, Materials of сonference: Precision Electromagnetic Measurements Digest,   Sydney, NSW, Australia, 05/14/2000 - 05/19/2000,  693 - 694 (2000).
  12. Khalilov E.N. Method  for  recording low-frequency  gravity  waves  and  device  for  the  measurement  thereof.  Patent of PCT. WO 2005/003818 A1., Geneva,  (13.01.2005).
  13. Khain V.E., Khalilov E.N. Tideless variations of gravity before strong  distant  earthquakes. Science Without Borders.  Volume 2. 2006/2006. ICSD/IAS H&E, Innsbruck, 319-339, (2006).
  14. Elsasser W.H. Convertion and stress propagation in the upper mantle. In: Appl. Modern Phys. Earth Planet. Inter. N.Y., Willey, 223-246, (1969).
  15. Lehner F.K., Li V.C., Rice J.R. Stress diffusion along rupturing  boundaries.  J.Geophys. Res., v.86, N B1, 6155-6169  (1981).

 

Book materials used in lectures:

Khalilov E.N. GLOBAL NETWORK FOR THE FORECASTING OF EARTHQUAKES - GNFE. INTERNATIONAL SYSTEM OF GEODYNAMICS MONITORING