caa a22 4500 477087566 CHVBK 20180405111507.0 cr unu---uuuuu 170330e19960101xx s 000 0 eng 10.1007/BF02606216 doi (NATIONALLICENCE)springer-10.1007/BF02606216 Solov'yov S. aut Simulation of heat exchange of a lithospheric platform in the zone of subduction. I. Statement of the problem [Elektronische Daten] [S. Solov'yov] The problems of numerical simulation of the processes of the thrust of an oceanic platform under a continental platform are considered. Numerical experiments on the calculation of the thermal state and evolution of subsidence of the oceanic platform in the zone of subduction are carried out. It is found that the maximum depth of subsidence of the oceanic platform does not exceed 720 km. Plenum Publishing Corporation, 1996 Journal of Engineering Physics and Thermophysics Kluwer Academic Publishers-Plenum Publishers 69/1(1996-01-01), 14-22 1062-0125 69:1<14 1996 69 10891 https://doi.org/10.1007/BF02606216 text/html Onlinezugriff via DOI 1 research-article jats NATIONALLICENCE 856 40 https://doi.org/10.1007/BF02606216 text/html Onlinezugriff via DOI NATIONALLICENCE 100 1- Solov'yov S. aut NATIONALLICENCE 773 0- Journal of Engineering Physics and Thermophysics Kluwer Academic Publishers-Plenum Publishers 69/1(1996-01-01), 14-22 1062-0125 69:1<14 1996 69 10891 Metadata rights reserved Springer special CC-BY-NC licence nationallicence BK010053 XK010053 XK010000 NATIONALLICENCE NATIONALLICENCE NL-springer