Enviar artigo por via de e-mail Thermal Model of Changes in the Thickness of the Continental Lithosphere over Time
- Autores: Trubitsyn A.P.1, Trubitsyn V.P.1,2
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Afiliações:
- Schmidt Institute of Physics of the Earth
- Institute of Earthquake Prediction Theory and Mathematical Geophysics
- Edição: Volume 481, Nº 2 (2018)
- Páginas: 1104-1107
- Seção: Geophysics
- URL: https://bakhtiniada.ru/1028-334X/article/view/193948
- DOI: https://doi.org/10.1134/S1028334X18080330
- ID: 193948
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Resumo
The results of numerical modeling for the increase and decrease in the thickness of a highly viscous continental lithosphere under whole-mantle convection on a time interval of 3.5 Ga were considered. It was found that the initial period of lithosphere growth took about 1.1 Ga, followed by a period of its slow thinning because of gradual heating of the mantle by several hundred degrees from the thermal insulation effect of the lithosphere.
Sobre autores
A. Trubitsyn
Schmidt Institute of Physics of the Earth
Autor responsável pela correspondência
Email: atrub@yandex.ru
Rússia, Moscow, 123810
V. Trubitsyn
Schmidt Institute of Physics of the Earth; Institute of Earthquake Prediction Theory and Mathematical Geophysics
Email: atrub@yandex.ru
Rússia, Moscow, 123810; Moscow, 113556
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