The model of whole mantle convection with formation of a long living reservoir feeding the mid-ocean ridge
- Авторлар: Evseev M.N.1, Trubitsyn V.P.1,2
-
Мекемелер:
- Institute of Physics of the Earth
- Institute of the Theory of Earthquake Prediction and Mathematical Geophysics
- Шығарылым: Том 476, № 1 (2017)
- Беттер: 1062-1065
- Бөлім: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/190841
- DOI: https://doi.org/10.1134/S1028334X17090197
- ID: 190841
Дәйексөз келтіру
Аннотация
This paper shows the results of numerical experiments that reproduce the main global structures in the mantle. In particular, it is shown how, under whole mantle convection, a subducting plate produces circulation currents feeding the mid-ocean ridge.
Авторлар туралы
M. Evseev
Institute of Physics of the Earth
Email: trub@ifz.ru
Ресей, Moscow, 123810
V. Trubitsyn
Institute of Physics of the Earth; Institute of the Theory of Earthquake Prediction and Mathematical Geophysics
Хат алмасуға жауапты Автор.
Email: trub@ifz.ru
Ресей, Moscow, 123810; Moscow, 113556
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