Abstract
Investigations of local geomagnetic field changes have been carried out in Middle Asia in the following regions: Tashkent, including Charvak reservoir, Fergana and Kyzyl-Kum. Since 1968, a variety of total field features have been observed there, including: (a) slow changes at separate stations, which may be explainable by compression or tension of individual earth’s crustal blocks; (b) a variety of field changes with amplitudes of a few gammas and periods of 0.5–2 years; (c) variations, which may be due to different conductivity of rocks; (d) anomalous changes in the fracture zones; (e) anomalous variations in the Charvak region, connected with reservoir filling. The amplitudes of these variations are 3–5 nT/year at Fergana, 8–9 nT/year at Kyzyl-Kum, 20–25 nT/year at Tashkent regions and up to 15–25 nT/year at Charvak reservoir area. Sometimes these anomalous changes are correlated with seismic activity (for example, Tashkent 1968 earthquakes).
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References
Abdullabekov, K.N. and S.Kh. Maksudov, Geomagnetic Field Variations in Seismoactive Regions, pp. 34–55, FAN Publishers, Tashkent, 1975.
Maksimovskikh, S.J. and V.A. Shapiro, Portable proton precession magnetometer of high accuracy T-MII, Geomagnetism y Aeronomia, XVI, 389–391, 1976.
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© 1979 Center for Academic Publications Japan
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Shapiro, V.A., Pushkov, A.N., Abdullabekov, K.N., Berdaliev, E.B., Muminov, M.Y. (1979). Geomagnetic Investigations in the Seismoactive Regions of Middle Asia. In: Fuller, M., Johnston, M.J.S., Yukutake, T. (eds) Tectonomagnetics and Local Geomagnetic Field Variations. Advances in Earth and Planetary Sciences, vol 5. Springer, Dordrecht. https://doi.org/10.1007/978-94-010-9825-0_5
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DOI: https://doi.org/10.1007/978-94-010-9825-0_5
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