Heat field of the north-west part of the Dnieper basin of the Dnieper-Donets depression
DOI:
https://doi.org/10.15407/dopovidi2014.01.097Keywords:
anomalies, Dnieper basin, heat fieldAbstract
The values of the deep heat flow were studied in 135 boreholes. The positive anomalies were detected. The anomalies have correlation with a fault zones in the crystalline foundation in south-west part regions. Single anomalous values occur in the north-east, but they are not combined into regional anomalies. A comparison of the results of geothermal studies with different physical fields was performed. The positive anomalies possibly correspond to the recent activation of this region.
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Gordienko V. V., Gordienko I. V., Zavgorodnjaja O. V., Usenko O. V. Thermal field of the territory of Ukraine. Kyiv: Znannia Ukrainy, 2002 (in Russian).
Gordienko V. V., Gordienko I. V., Zavgorodnjaja O. V., Kovachikova S., Logvinov I. M., Pek Yu., Tarasov V. N., Usenko O. V. Dnieper-Donets Basin (geophysics, deep processes). Kyiv: Korvin pres, 2006 (in Russian).
Ivanyuta M. M. et al. (Eds.). Atlas of oil and gas Ukraine. In 6 vols. Vol. 1-6. Lviv, 1998–1999. (in Ukrainian).
Verkhovtsev V. G. The vertical latest modern crustal movements territory of Ukraine, their relationship with the ring and linear structures. In: Power of Earth, its geological and ecological displays, scientific and practical use. Kyiv: VPC “Kyivskyi universytet”, 2006: 129–137 in Ukrainian).
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