RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 15, ES4002, doi:10.2205/2015ES000556, 2015
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° |
Citation: Parphenuk O. I. (2015), Uplifts formation features in continental collision structures (evolution modeling), Russ. J. Earth Sci., 15, ES4002, doi:10.2205/2015ES000556.
Copyright 2015 by the Geophysical Center RAS.