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Relevant bibliographies by topics / Telluric-magnetotelluric Reconnaissance Telluric-magnetotelluric Measurements

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Academic literature on the topic 'Telluric-magnetotelluric Reconnaissance Telluric-magnetotelluric Measurements'

Author: Grafiati

Published: 6 September 2023

Last updated: 31 July 2025

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Journal articles on the topic "Telluric-magnetotelluric Reconnaissance Telluric-magnetotelluric Measurements"

1

Prystai, A. M., and V. O. Pronenko. "Improving of electrical channels for magnetotelluric sounding instrumentation." Geoscientific Instrumentation, Methods and Data Systems 4, no. 2 (2015): 149–54. http://dx.doi.org/10.5194/gi-4-149-2015.

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Abstract. The study of the deep structure of the Earth's crust is of great interest for both applied (e.g. mineral exploration) and scientific research. For this the electromagnetic (EM) studies which enable one to construct the distribution of electrical conductivity in the Earth's crust are of great use. The most common method of EM exploration is magnetotelluric sounding (MT). This passive method of research uses a wide range of natural geomagnetic variations as a powerful source of electromagnetic induction in the Earth, producing telluric current variations there. It includes the measurem

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2

Prystai, A. M., and V. O. Pronenko. "Improving of electrical channels for magnetotelluric sounding instrumentation." Geoscientific Instrumentation, Methods and Data Systems Discussions 5, no. 1 (2015): 63–81. http://dx.doi.org/10.5194/gid-5-63-2015.

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Abstract. The study of deep structure of the Earth's crust is of great interest for both applied (e.g. mineral exploration) and scientific research. For this the electromagnetic (EM) studies which enable to construct the distribution of electrical conductivity in the Earth's crust are of great use. The most common method of EM exploration is magnetotelluric sounding (MT). This passive method of research uses a wide range of natural geomagnetic variations as a powerful source of electromagnetic induction in the Earth, producing there telluric currents variations. It includes the measurements of

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3

Doumouya, V., J. Vassal, Y. Cohen, O. Fambitakoye, and M. Menvielle. "Equatorial electrojet at African longitudes: first results from magnetic measurements." Annales Geophysicae 16, no. 6 (1998): 658–66. http://dx.doi.org/10.1007/s00585-998-0658-9.

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Abstract. In the framework of the French participation in the International Equatorial Electrojet Year (IEEY), ten magnetotelluric stations were installed between November 1992 and November 1994 along a 1200-km-long meridian profile, between Lamto (latitude 6.2°N, Côte d'Ivoire) to the south and Tombouctou (latitude 16.7°N, Mali) to the north. These stations measured digitally the three components of the magnetic field and the two components of the telluric electric field, and operated over a period of 20 months. The magnetic data is used to study the features of the equatorial electrojet (EEJ

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4

Hutton, V. R. S. "Magnetic, telluric and magnetotelluric measurements at the Travale test site, Tuscany, 1980–1983: An overview." Geothermics 14, no. 5-6 (1985): 637–44. http://dx.doi.org/10.1016/0375-6505(85)90039-2.

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5

Berktold, A. J., H. J. Dittus, K. H. Eigner, and U. Teufel. "Investigation of the geothermal anomaly of Travale (Tuscany) by telluric, magnetotelluric and geomagnetic deep sounding measurements." Geothermics 14, no. 5-6 (1985): 663–72. http://dx.doi.org/10.1016/0375-6505(85)90042-2.

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6

Jones, Alan G. "Static shift of magnetotelluric data and its removal in a sedimentary basin environment." GEOPHYSICS 53, no. 7 (1988): 967–78. http://dx.doi.org/10.1190/1.1442533.

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Previous modeling investigations of the static shift of magnetotelluric (MT) apparent resistivity curves have limited appeal in that the electric fields used were point measurements, whereas field observations are of voltage differences. Thus, inhomogeneities of dimension of the order of the electrode line length could not be investigated. In this paper, by using a modeling algorithm that derives point voltages rather than point electric fields, I consider the effect on the MT responses of local near‐surface distorting structures, which are both outside of, and inside, the telluric electrode a

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7

Вишнев, В. С., and П. Ф. Астафьев. "ABOUT THE VERTICAL COMPONENT OF THE ELECTRIC MAGNETO-TELLURIC FIELD STRENGTH IN THE RANGE SHORT-PERIOD OSCILLATIONS." Уральский геофизический вестник, no. 3(49) (September 30, 2022): 14–21. http://dx.doi.org/10.25698/ugv.2022.3.2.14.

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Рассмотрены методические приемы полевого эксперимента по изучению вклада галь- ванического возбуждения земных недр геомагнитными вариациями в суммарное естественное элек- тромагнитное поле диапазона короткопериодических колебаний. Произведено сравнение скважинных распределений отношений вертикальных составляющих электрической напряженности естественного и искусственно созданного полей к их горизонтальным составляющим. Сделано предположение о том, что доля вклада этого типа возбуждения Земли (по сравнению с индукционным возбуждением) на тер- риториях, относящихся к средним широтам, много меньше

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8

Käufl, J. S., A. V. Grayver, M. J. Comeau, et al. "Magnetotelluric multiscale 3-D inversion reveals crustal and upper mantle structure beneath the Hangai and Gobi-Altai region in Mongolia." Geophysical Journal International 221, no. 2 (2020): 1002–28. http://dx.doi.org/10.1093/gji/ggaa039.

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SUMMARY Central Mongolia is a prominent region of intracontinental surface deformation and intraplate volcanism. To study these processes, which are poorly understood, we collected magnetotelluric (MT) data in the Hangai and Gobi-Altai region in central Mongolia and derived the first 3-D resistivity model of the crustal and upper mantle structure in this region. The geological and tectonic history of this region is complex, resulting in features over a wide range of spatial scales, which that are coupled through a variety of geodynamic processes. Many Earth properties that are critical for the

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9

Hermance, J. F., and G. A. Neumann. "Magnetic variations in the reconnaissance of sedimentary basins: Field procedure and generalized inversion of short‐period data from the Rio Grande rift." GEOPHYSICS 55, no. 12 (1990): 1567–76. http://dx.doi.org/10.1190/1.1442808.

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The magnetic variation (MV) technique employs magnetic transients from natural sources in the magnetosphere to delineate geologic structures in the earth’s interior based on their electrical properties. By measuring only the magnetic field at each site, and not the electric field as required for magnetotelluric (MT) studies, a site can be set up quickly, and often in places which might be quite unsuitable for MT measurements. This generally allows one to execute MV surveys in culturally developed areas or in rugged and logistically difficult terrain at much closer site spacings than those used

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10

V. A. Pilipenko, M. Vellante, S. Anisimov, M. De Lauretis, E. N. Fedorov, and U. Villante. "Multi-component ground-based observation of ULF waves: goals and methods." Annals of Geophysics 41, no. 1 (1998). http://dx.doi.org/10.4401/ag-3794.

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A revival of the combined magnetic and telluric electric measurements at magnetic observatories is suggested.A number of problems, where such observations might be very helpful, are outlined: 1) the account for the resonance structure of the ULF field during the magnetotelluric probing of low-conductive geoelectrical structures; 2) the hydromagnetic diagnostics of the magnetospheric plasma distribution; 3) the discrimination of ionospheric and seismic contributions in anomalous ULF signals possibly related with earthquakes. The experimental apparatus for telluric current measurements, which ha

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Books on the topic "Telluric-magnetotelluric Reconnaissance Telluric-magnetotelluric Measurements"

1

J, Berktold A., and Commission of the European Communities. Directorate-General for Science, Research and Development., eds. Investigation of the geothermal anomaly of Travale/Tuscany by telluric, magnetotelluric and geomagnetic deep sounding measurements. Commission of the European Communities, 1986.

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