А.Д. Дучков,В.Т.Балобаев,Б.В.Володько,В.Н.Девяткин,С.В.Лысак,Ю.М.Пузанков,А.Д.Ножкин, Л.С. Соколова,В.И.Березкин,Л.М.Богомолова,Е.А.Ботулу,Р.П.Дорофеева,В.Л.Дук,А.С.Егоров,А.Н.Зедгенизов,А.Н.Зуй,В.И.Кицул,А.М.Ковешников,А.Б.Котов, А.Р. Курчиков,В.И.Медведев, Н.В. Попов,В.Г.Русаков,А.П.Смелов,В.В.Стогний,О.М.Туркина,Н.А.Шендер
Сериальное издание: Труды ОИГГМ СО РАН
Место издания: Новосибирск
, Год издания: 1994
Аннотация
New data on geothermic parameters of the upper layer of the Earth's crust (down to 5 km) for Asian part of Russia are summarized in the monograph. Information on heat flow and temperature of cryosphere and underlying rocks both in vast blocks of the Earth's crust in the platform areas of Siberia (chap.1, 1.1-1.2) and within selected oil fields (chap.2) is reported and analyzed. Radiochemical data on the Aldan Shield and Kamchatka region (chap.3), being the basis for estimation of space variations of intensity of radiogenic heat generation in the Earth's crust are considered. A modern geocryological state in the West Siberia is discussed, a scenario of its variations under conditions of global warming of climate is suggested (chap.1, 1.3).
индекс в базе ИАЦ: 013906
