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dc.contributor.authorZui, V. I.-
dc.contributor.authorTsalko, P. B.-
dc.contributor.authorZhuk, M. S.-
dc.date.accessioned2015-04-25T14:54:30Z-
dc.date.available2015-04-25T14:54:30Z-
dc.date.issued2000-
dc.identifier.urihttp://elib.bsu.by/handle/123456789/113389-
dc.description.abstractResults of regional investigations of terrestrial temperature field within intersynclinal local structures of so-called “tortoise-shell type” are discussed. Such geological structures were distinguished within the central part of the Pripyat Trough. Heat flow density estimates are fulfilled for a number of drillholes. The influence of hydrogeologic conditions, salt tectonics, mineralogical composition of rocks in the platform cover are discussed.-
dc.language.isoruru
dc.subjectЭБ БГУ::ЕСТЕСТВЕННЫЕ И ТОЧНЫЕ НАУКИ::Геологияru
dc.titleHeat Flow Within Local Intersynclinal Structures Of the Tortoise-Shell TypeEru
dc.typepreprintru
Appears in Collections:Кафедра региональной геологии (статьи)

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