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1
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0002043371
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The correction for heating-induced chemical alterations in archaeomagnetic determinations of the ancient geomagnetic field intensity
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Burakov, K.S. and Nachasova, I.E., The Correction for Heating-Induced Chemical Alterations in Archaeomagnetic Determinations of the Ancient Geomagnetic Field Intensity, Izv. Akad. Nauk SSSR, Fiz. Zemli, 1985, no. 10, pp. 93-96.
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Application of gradient and regularization methods to the determination of signal and trend parameters
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Moscow
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Filippov, S.V.1
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Methods of recognition and the space-time structure of 20-year variations in the geomagnetic field from data of the worldwide observatory network
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Moscow
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Filippov, S.V. and Rotanova, N.M., Methods of Recognition and the Space-Time Structure of 20-Year Variations in the Geomagnetic Field from Data of the Worldwide Observatory Network, Preprint of Inst. Terrestrial Magnetism, Ionosphere and Radiowave Propagation, USSR Acad. Sci.,Moscow, 1985, no. 3 (692).
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Stratigraphy of upper layers of the Northern Anau Hill
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Altyn-depe in the eneolithic epoch
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Geomagnetic archaeointensity in the 5th Millennium B.C. in Northern Mesopotamia
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Nachasova, I.E. and Burakov, K.S., Geomagnetic Archaeointensity in the 5th Millennium B.C. in Northern Mesopotamia, Geomagn. Aeron., 1995, vol. 35, no. 3, pp. 131-137.
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Geomagnetic field variations in Central Asia in the last 2000 years: The analysis of worldwide data
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Nachasova, I.E. and Burakov, K.S., Geomagnetic Field Variations in Central Asia in the Last 2000 Years: The Analysis of Worldwide Data, Geomagn. Aeron., 1997a, no. 6, pp. 150-157.
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The geomagnetic field intensity in Central Asia in the 2nd to 1st Millenniums B.C.
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Nachasova, I.E. and Burakov, K.S., The Geomagnetic Field Intensity in Central Asia in the 2nd to 1st Millenniums B.C., Fiz. Zemli, 1997b, no. 7, pp. 33-38.
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The 8000-year geomagnetic intensity variation
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Nachasova, I.E. and Burakov, K.S., The 8000-Year Geomagnetic Intensity Variation, Geomagn. Aeron., 1997c, vol. 37, no. 1, pp. 167-173.
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