Plate tectonics and the Alpine orogeny: implications of thermometric and kinematic analyses of the upper and lower boundaries of the Pennine Zone in the Central Alps

Author(s):  
Jason B Price ◽  
Brian P Wernicke
2020 ◽  
Vol 42 (3) ◽  
pp. 271-282
Author(s):  
OLEG IVANOV

The general characteristics of planetary systems are described. Well-known heat sources of evolution are considered. A new type of heat source, variations of kinematic parameters in a dynamical system, is proposed. The inconsistency of the perovskite-post-perovskite heat model is proved. Calculations of inertia moments relative to the D boundary on the Earth are given. The 9 times difference allows us to claim that the sliding of the upper layers at the Earth's rotation speed variations emit heat by viscous friction.This heat is the basis of mantle convection and lithospheric plate tectonics.


2006 ◽  
Vol 17 (7) ◽  
pp. 209-253
Author(s):  
Pavel M. Goryainov ◽  
G. Yu. Ivanyuk ◽  
A. O. Kalashnikov
Keyword(s):  

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