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About the so-called “magnetic tellurics” — Comment on “long period electromagnetic induction vectors in a sedimentary back-arc basin” (Carpatho-Pannonian Basin) by A Ádám and A Koppán

Annual, monthly, weekly and diurnal distribution of Carpathian (1964–2004) and M>7 earthquakes worldwide (1900–2004) and seeking for the effect of the Moon

Seismicity of the Western-Carpathians

Acta Geodaetica et Geophysica Hungarica : Volume 40, Issue 2, May 2005

Acta Geodaetica et Geophysica Hungarica : Volume 40, Issue 1, March 2005

Acta Geodaetica et Geophysica Hungarica : Volume 39

Acta Geodaetica et Geophysica Hungarica : Volume 38

Acta Geodaetica et Geophysica Hungarica : Volume 37

Acta Geodaetica et Geophysica Hungarica : Volume 36

Acta Geodaetica et Geophysica Hungarica : Volume 35

Acta Geodaetica et Geophysica Hungarica : Volume 34

Acta Geodaetica et Geophysica Hungarica : Volume 33

Acta Geodaetica et Geophysica Hungarica : Volume 32

Results of tidal research

Content Provider	Springer Nature Link
Author	Mentes, Gy.
Copyright Year	2005
Abstract	At the Geodetic and Geophysical Research Institute of the Hungarian Academy of Sciences the tidal research was started in the mid-sixties of the last century. At first, measurements by horizontal pendulums (Tomaschek-Ellenberger, Melchior) were carried out. At the beginning of the 70’s a new horizontal pendulum with capacitive transducer was developed. By means of this pendulum tidal measurements were carried out at the Geodynamical Observatory in Sopronbánfalva and local geodynamical movements were monitored in a coal mine in Pécs and at our nuclear power plant in Paks.At the beginning of the 90’s a quartz tube extensometer with capacitive transducer was installed at the Geodynamical Observatory in Sopron and in the uranium mine in Pécs. The extensometers in Budapest installed in the early 80’s, the extensometer in Výhne (Slovakia) were mounted with capacitive transducers. New, in-situ calibration method was developed at our institute and all of these extensometers were recalibrated by the new calibration device.A microbarograph of high resolution was also developed for the study of atmospheric tide in 1991. The investigation of the connection between air pressure variations and geodynamical phenomena has been carried out since 1992.This paper presents the developed instruments and the results obtained by these instruments.
Starting Page	293
Ending Page	305
Page Count	13
File Format	PDF
ISSN	12178977
Journal	Acta Geodaetica et Geophysica Hungarica
Volume Number	40
Issue Number	3-4
e-ISSN	15871037
Language	English
Publisher	Springer Netherlands
Publisher Date	2013-02-27
Publisher Institution	Quarterly of the Hungarian Academy of Sciences
Publisher Place	Dordrecht
Access Restriction	Subscribed
Subject Keyword	magnetostrictive coil capacitive transducer atmospheric tide horizontal pendulum in-situ calibration microbarograph tectonic movements Geophysics/Geodesy extensometer Earth tide
Content Type	Text
Resource Type	Article
Subject	Building and Construction Geology Geophysics

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Results in physical geodesy

Atmospheric tide obtained by the microbarograph developed at the Geodetic and Geophysical Research Institute of the Hungarian Academy of Sciences

Comparison of extensometric results measured in the Vyhne Tidal Station (Slovakia) and in the Sopronbánfalva Geodynamic Observatory (Hungary)

On origins of geodynamics and of modern seismology

Local effects disturbing the monitoring of tectonic movements of the Mecsekalja fault by shallow deep borehole tiltmeters in Hungary

Investigation of the possibility of using tidal signals for health monitoring of objects

Spatial and temporal variations of the correlation coefficient between M2 and S2 earth tides components and earthquake occurrences for the intermediate-depth seismic activity zones

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Results of tidal research

Similar Documents

Results in physical geodesy

Atmospheric tide obtained by the microbarograph developed at the Geodetic and Geophysical Research Institute of the Hungarian Academy of Sciences

Comparison of extensometric results measured in the Vyhne Tidal Station (Slovakia) and in the Sopronbánfalva Geodynamic Observatory (Hungary)

On origins of geodynamics and of modern seismology

Local effects disturbing the monitoring of tectonic movements of the Mecsekalja fault by shallow deep borehole tiltmeters in Hungary

Investigation of the possibility of using tidal signals for health monitoring of objects

Spatial and temporal variations of the correlation coefficient between M2 and S2 earth tides components and earthquake occurrences for the intermediate-depth seismic activity zones

Evolution of angular momenta and energy of the Earth-Moon system

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Results of tidal research