Geodynamic Evolution Model of the Major Structures of Amerasian Basin
- Авторлар: Lobkovsky L.I.1, Garagash I.A.2, Alekseev D.A.1,2
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Мекемелер:
- Shirshov Institute of Oceanology
- Schmidt Institute of Physics of the Earth
- Шығарылым: Том 480, № 2 (2018)
- Беттер: 753-757
- Бөлім: Geophysics
- URL: https://journal-vniispk.ru/1028-334X/article/view/193366
- DOI: https://doi.org/10.1134/S1028334X18060065
- ID: 193366
Дәйексөз келтіру
Аннотация
We have analyzed the geodynamic evolution of the lithosphere and upper mantle of the Amerasian basin based on the stress-strain state simulation. It is shown that the asthenospheric spreading in the return upflow region of the mantle convection, results in formation of two local uplifts, which can be interpreted as Lomonosov Ridge and Mendeleev/Alfa Ridge. The further long-term action of the mantle convection leads to formation of Makarov and Podvodnikov Basins.
Авторлар туралы
L. Lobkovsky
Shirshov Institute of Oceanology
Email: alexeevgeo@gmail.com
Ресей, Moscow, 117218
I. Garagash
Schmidt Institute of Physics of the Earth
Email: alexeevgeo@gmail.com
Ресей, Moscow, 123810
D. Alekseev
Shirshov Institute of Oceanology; Schmidt Institute of Physics of the Earth
Хат алмасуға жауапты Автор.
Email: alexeevgeo@gmail.com
Ресей, Moscow, 117218; Moscow, 123810
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