Мақаланы E-mail арқылы жіберу Thermal Model of Changes in the Thickness of the Continental Lithosphere over Time
- Авторлар: Trubitsyn A.P.1, Trubitsyn V.P.1,2
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Мекемелер:
- Schmidt Institute of Physics of the Earth
- Institute of Earthquake Prediction Theory and Mathematical Geophysics
- Шығарылым: Том 481, № 2 (2018)
- Беттер: 1104-1107
- Бөлім: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/193948
- DOI: https://doi.org/10.1134/S1028334X18080330
- ID: 193948
Дәйексөз келтіру
Ашық рұқсат
Рұқсат берілді
Тек жазылушылар үшін
Аннотация
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.
Авторлар туралы
A. Trubitsyn
Schmidt Institute of Physics of the Earth
Хат алмасуға жауапты Автор.
Email: atrub@yandex.ru
Ресей, Moscow, 123810
V. Trubitsyn
Schmidt Institute of Physics of the Earth; Institute of Earthquake Prediction Theory and Mathematical Geophysics
Email: atrub@yandex.ru
Ресей, Moscow, 123810; Moscow, 113556
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