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Поток Внетриземного Тепла В монгольской Народной Республике

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Results of field investigations are presented, which have enabled us for the first time to determined, more or less accurately, the heat flow at three points, distributed near the north and south boundary and in the central part of the Mongolian People's Republic.

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Лumерamурa

  1. Г. Карслоу, Д. Егер: Теплопроводность твердых тел. Наука, М. 1964.

  2. Ю. Г. Шасткевич: Многолетнемерзлые породы высокогорной части хребта Удокан и условия формирования их температурного режима. Геокриологические условия Забайкальского Севера, Наука, М. 1966.

  3. Е. А. Любимова, В. А. Шелягин: Тепловой поток через дно оз. Байкал. ДАН СССР, 171 (1966), 1321.

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  1. Ор¶rt;енa Тру¶rt;овоsо Крaсноsо Знaменu Инсmumуm мерзлоmове¶rt;енця СО АН СССР, Якуmск

    Ю.Г Щасткевич & С.И Заболотник

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  1. Ю.Г Щасткевич
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  2. С.И Заболотник
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Щасткевич, Ю., Заболотник, С. Поток Внетриземного Тепла В монгольской Народной Республике. Stud Geophys Geod 19, 197–200 (1975). https://doi.org/10.1007/BF01635428

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  • DOI: https://doi.org/10.1007/BF01635428

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