电邮这篇文章 Thermal Model of Changes in the Thickness of the Continental Lithosphere over Time
- 作者: Trubitsyn A.P.1, Trubitsyn V.P.1,2
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隶属关系:
- Schmidt Institute of Physics of the Earth
- Institute of Earthquake Prediction Theory and Mathematical Geophysics
- 期: 卷 481, 编号 2 (2018)
- 页面: 1104-1107
- 栏目: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/193948
- DOI: https://doi.org/10.1134/S1028334X18080330
- ID: 193948
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详细
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.
作者简介
A. Trubitsyn
Schmidt Institute of Physics of the Earth
编辑信件的主要联系方式.
Email: atrub@yandex.ru
俄罗斯联邦, Moscow, 123810
V. Trubitsyn
Schmidt Institute of Physics of the Earth; Institute of Earthquake Prediction Theory and Mathematical Geophysics
Email: atrub@yandex.ru
俄罗斯联邦, Moscow, 123810; Moscow, 113556
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