RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 16, ES6006, doi:10.2205/2016ES000589, 2016


Table 2. Temperature values (in ° C) under the middle point of the uplift near the end of shortening ($t = 19.4$ Ma) – the left columns, at postcollision stage ($t = 62$ Ma) – the right columns. See text for the details
$H_{\mathrm{low}} = 1.5$ $\mu$W/m$^3$ $H_{\mathrm{norm}} = 2.0$ $\mu$W/m$^3$$H_{\mathrm{high}} = 2.5$ $\mu$W/m$^3$
$La_{\mathrm{low}} = 2.0$ W/m K 685/730 780/840 715/755 840/890 750/885 885/920
$La_{\mathrm{norm}} = 2.5$ W/m K 630/700 700/770 665/720 745/810 700/740 780/840
$La_{\mathrm{high}} = 3.0$ W/m K 590/670 615/705 620/690 670/750 650/710 710/780

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Citation: Parphenuk O. I. (2016), Thermal regime and heat transfer during the evolution of continental collision structures, Russ. J. Earth Sci., 16, ES6006, doi:10.2205/2016ES000589.


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