RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 15, ES4002, doi:10.2205/2015ES000556, 2015


Table 1.
Upper crust ($i = 3$) Lower crust ($i = 1$) Lithospheric upper mantle ($i =2$)
Specific heat capacity ($c$, J/kg K) $10^3$ $10^3$ $10^3$
Thermal conductivity ($\lambda$, W/m K) 2.5 3 4
Heat generation rate ($H$, $\mu$W/m$^3$) 1.5; 2.0; 2.5 1.1 0.08
Density ($\rho$, kg/m$^3$) 2750 3000 3300
Effective viscosity ($\mu$, Pa s) $5\times 10^{20}- 10^{22}$ $5\times 10^{21}- 10^{23}$
Layer thickness ($h$, km) 20 20 80
Dip angle of fault zone 15–30°

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Citation: Parphenuk O. I. (2015), Uplifts formation features in continental collision structures (evolution modeling), Russ. J. Earth Sci., 15, ES4002, doi:10.2205/2015ES000556.


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