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New experimental data on temperature, thermogradient and thermal conductivity have been obtained for the SG-3 well and 22 wells of annular space have been processed. An influence of technogene factors on the geothermic characteristics of stratum was estimated. The new data on the thermal regime parameters, character and degree of an influence of the mass and transfer processes for the depth interval of 0-9000 m were obtained. It was shown that even in the depth interval of 6500-9000 m the heat transfer process differs from the conductive one. The crustal thermal regime estimation for deep horizones not reached by the SG-3 drilling differs from the previous forecast data signifivcantly.
New experimental data on temperature and thermogradient distribution along the Vorotilovo deep and Ural superdeep wells were obtained. The heat flow density distribution along the Ural superdeep well SG-4 was calculated within the depth interval of 0-4800 m.
The new parameter - the ratio of temporal variations of thermogradient - and thermogradient - thermal conductivity correlation analyses approach were suggested to distinguish permeable zones of strata. The approach was used for the Kola and Ural well section study.
Numerous measurements of thermal conductivity were carried out for the Timano-Pechora and Kolva deep well sections within depth intervals not studied before. New data about thermal anisotropy of rocks and values and vertical variations of heat flow density and heat and mass transfer processes were obtained.
The degree of paleoclimate influence on vertical variations of geothermic parameters under permafrost zones was estimated for sections of the Tyumen and Kolva wells.
The opportunities for an improvement of functional and metrological parameters of the optical scanning instruments were found out.
The study of an opportunity to use the new theoretical models of effective thermal conductivity to forecast the thermal properties on minelarogical composition and structural-textural data was performed.
Geothermal characteristics of the Vorotilovo deep borehole drilled into the Puchezh-Katunk impact structure , , , Tectonophysics
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Sharp increase in heat flow density along the Ural superdeep borehole CG-4 , Abstracts of the 29th General Assembly of the IASPEI (1997) 249
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An increase in heat flow density from measurements in deep boreholes: an actual result or effect of experimental errors? Abstracts of the 29th General Assembly of the IASPEI (1997) 417
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The effect of rock anisotropy on the estimation of heat flow density for the Kolva, Tyumen, and Kola deep borehole Abstracts of the 29th General Assembly of the IASPEI (1997) 420
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Optical scanning technology for nondestructive contactless measurements of thermal conductivity and diffusivity of solid matters Proceedings of the 4th World Conference on Experimental Heat Transfer, Fluid Mechanics and Thermodynamics (1997) 109-117
