THERMAL STATE OF LITHOSPHERE IN MONGOLIA
S.V. Lysak and R.P. Dorofeeva
Institute of the Earth's Crust, Siberian Branch of the RAS, 128 ul. Lermontova, Irkutsk, 664033, Russia
Keywords: Temperature, geothermal gradient, thermal conductivity, heat production, heat flow, hot springs, tectonic activity, thermal evolution
Pages: 893-903
Abstract
The thermal state of lithosphere in Mongolia has been modeled on the basis of measured regional heat flows and predicted temperatures at depths of 0 to 50 km. The highest temperatures of 1100-1200
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