Strategy of Development of Largescale Research Infrastructures of the Russian Federation

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Strategy of Development of Large-scale Research
Infrastructuresof the Russian Federation
Cooperation with the European Unitn
September 7-8, 2009 Copenhagen -
Denmark

• Joint Use Center for Vibroseismic Sources
• Kuban State University

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• Joint Use Center for Heavy Vibroseismic Sources
  was established in 2000.The Association for
  Seismic Protection of the Black Sea Economic
  Cooperation Member States was founded the same
  year and took this Center as Joint Used.It is
  equipped with four different types of
  vibroseismic sources.Two heavy 100 t stationary
  vibroseismic TV-100 sources.American mobile
  vibroseismic Y-300 source.Two American 17 t
   mobile vibroseismic A-1100 sources.Russian 10
  t mobile vibroseismic CT-10 source.Moreover,
  the Center is equipped with the hardware complex,
  providing receiving and processing of seismic
  data and signals excited by vibroseismic sources.

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KubSU testing ground. Heavy TV-100 geoseismic
vibrators with a dynamic force of 100 tons each
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KubSU testing ground. American 30-t experimental
Y-3000 geosesimic vibrator, donated by Tengasco,
an American oil company
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KubSU testing ground. American 17-t A- 1100
geosesimic vibrator, one of two vibrators donated
by Tengasco, an American oil company
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KubSU testing ground.
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KubSU testing ground. 10-t ??-10 geosesimic
vibrator.
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Joint Use Center for Heavy Vibroseismic
Sourcesprovides service for next organizaitions

• 1.Oil Company Priazovneft
• 2.State Scientific Center of the Russian
  Federation Federal State Unitary Geological
  Enterprise South Scientific-Production
  Association for Marine Exploration3.Schmidt
  Institute of Earth Physics of the Russian Academy
  of Science
• 4.Adyghe State University
• 5.Southern Research Center of the Russian Academy
  of Science
• 6.Institute of Computational Mathematics and
  Mathematical Geophysics of the RAS Siberian
  Branch
• 7. Olimpstroi.

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Geoinformational systemSeismozonaKuban
State Universitywww.kubsu.ru
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• Development of GIS Seismozona consists in the
  construction of the fields of litosphere plates
  Stressed-deformed state taking into account all
  basis factors

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Earthquake forecasting is one of the unsettled
problems of the humanity. Earthquakes take a
heavy toll of human lives and bring tremendous
destructions
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Currently the only reliable earthquake precursor
is abnormal behavior ofanimals.
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Current perception of underground processes
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Current perception of underground processes
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???????????????? ????? ???????????? - ??????????
????????????? ?????????????? ???????Under the
auspices of the Administration of the Krasnodar
region, Russian and foreign foundations and
organizations, Kuban State University is
developing a Seismozona geoinformation system,
which is unique in the world. The concept was
reported at the Russian Academy of Sciences, at
the joint session of the Russian Ministry for
Emergency Situations and Ministry of Science,
during seminars and conferences in the USA,
Germany, Italy, Sweden, Greece, and Turkey. The
concept is based on the differential
factorization method, i.e. specially developed
mathematical tools
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Hydrometeorologists forecast weather using
satellite information about cloud drift
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Hydrometeorologists forecast weather using
satellite information about cloud drift
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Hydrometeorologists forecast weather using
satellite information about cloud drift
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The Earth crust is regarded as a deformable
elastic shell on a viscous-elastic sphere or a
half-space. Increase of seismic activity is the
growth of stress concentration.
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• Possibility of assessing stressed-deformable
  state of lithosphere plates
• Seismozona Model

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Some factors acting on the stressed-deformable
state of lithosphere plates
Faults
Ocean
Granite
Basalt
Upper mantle
Gravity field, Earth's rotation, preliminary
stress, temperature stress, Moons gravity,
atmosphere pressure, vertical and horizontal
movement of plates, solar activity, vibrations of
the sea area, activity of the upper mantle (at
the Mohorovicic discontinuity)
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Breaks of the Krasnodar Region
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Vibroseis acquisition method
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Segments of seismic profiles constructed
through the whole thickness of the lithosphere
plate by US scientists (Ohio, Prof. R. Williams,
University of Tennessee, Knoxville)
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.KubSU testing ground. American 30-t
experimental Y-3000 geosesimic vibrator, one of
several vibrators donated by Tengasco, an
American oil company
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KubSU testing ground. Vibroseis acquisition
process.
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KubSU testing ground. American NX-48 seismograph
(Silicon Valley, San-Jose) with manifold research
possibilities
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Study of the Earths internal structure and
tectonic properties
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American NX-48 seismographs purchased by tender
by the Administration and Legislative Assembly of
the Krasnodar region and Russian Ministry of
Education
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Petrel program donated to KubSU by French
Schlumberger makes it possible to construct 3D
profiles of lithosphere plates while processing
vibroseis information
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Construction of 3D profiles of lithosphere
plates while processing vibroseis information
requires the application of powerful servers
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• Possibility of organizing monitoring of
• lithosphere plates strain

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• Possibility of obtaining data about daily
  vertical displacements of a lithosphere plate

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???????? ??????????? ?????Hydrodeformational
investigation of vertical movements of the
Earth's surface
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???????????? ?????????????? ??????????? ???
?????? ? ??????? ??????? ????Study of
deformation processes in Southern Russia with the
application of the RITM system
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????Geomonitoring scheme of the Krasnodar region
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• Possibility of obtaining data about horizontal
  displacements of lithosphere plates

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GPS antenna of the Gelendzhik Yuzhmorgeologiyas
satellite geodynamic station to measure
horizontal displacements of the Earth
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Khadyzhensk satellite geodynamic station
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Field geodesic kit GPS/GLONASS
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The Black Sea Economic Cooperation region,
movement of lithosphere plates
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The Black Sea Economic Cooperation region,
movement of lithosphere plates
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The Black Sea Economic Cooperation region,
movement of lithosphere plates
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• Possibility of measuring tilt, tension and
  microseisms of lithosphere plates

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High-precision tiltmeter at the KubSU seismic
laboratory
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Continuous record of the lithosphere plate tilt
alteration
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Continuous record of the lithosphere plate tilt
alteration
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Continuous record of the lithosphere plate tilt
alteration
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Continuous record of the lithosphere plate tilt
alteration
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Continuous record of the lithosphere plate tilt
alteration
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??????????? ?????? ????????? ???????? ???????????
?????Continuous record of the lithosphere plate
tilt alteration
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??????????? ?????? ????????? ???????? ???????????
?????Continuous record of the lithosphere plate
tilt alteration
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??????????? ?????? ????????? ???????? ???????????
?????Continuous record of the lithosphere plate
tilt alteration
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??????????? ?????? ????????? ???????? ???????????
?????Continuous record of the lithosphere plate
tilt alteration
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Possibility of seismic monitoring using
satellite-assisted digital stations KubSU seismic
laboratory
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?????Equipment at the KubSU seismic laboratory
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Equipment at the KubSU seismic laboratory
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Research equipment of the KubSU seismic
laboratory used for the above purposes
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Research equipment of the KubSU seismic
laboratory used for the above purposes
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A microseism continuously registered by
geophysical equipment
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Seismic situation is calm
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An earthquake occurred. Its location, time and
coordinates are determined by the KubSU
satellite-assisted seismic station
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• Possibility of studying electric resistance of
  deep-seated medium, from 15 m to 150 km

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Fifth-generation MTU-5 magnetotelluric station
produced by Phoenix Geophysics Ltd., Canada
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Magnetotelluric experiments held at the testing
ground of Kuban State University and RAS Southern
Research Center
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Magnetotelluric experimentsusing station MTU-5?
Phoenix.
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The results of the experiments
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The results of the experiments
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The results of the experiments
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• Possibility of research works and computations
  automatization using GIS-technologies

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A possibility of calculating stressed-deformable
state of lithosphere plates according to the
given parameters on the surface
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Stress concentration in two plates
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Stress concentration in three plates
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Stress concentration in three plates
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Stress concentration in three plates
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Stress concentration in four plates
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• Thank you
• very much!