Modelling of thermal stratification at the top of a planetary core: Application to the cores of Earth and Mercury and the thermal coupling with their mantles
Author:
Publisher
Elsevier BV
Subject
Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics
Reference53 articles.
1. Geomagnetic fluctuations reveal stable stratification at the top of the Earth’s core;Buffet;Nature,2014
2. Stratification of the top of the core due to chemical interactions with the mantle;Buffet;J. Geophys. Res. Solid Earth,2010
3. Evidence for MAC waves at the top of Earth’s core and implications for variations in length of day;Buffet;Geophys. J. Int.,2016
4. A dynamo explanation for Mercury’s anomalous magnetic field;Cao;Geophys. Res. Lett.,2014
5. Non-ideal liquidus curve in the Fe-S system and Mercury’s snowing core;Chen;Geophys. Res. Lett.,2008
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1. Thermal and magnetic evolution of Mercury with a layered Fe-Si(-S) core;Earth and Planetary Science Letters;2024-09
2. Mantle Mineralogy of Reduced Sub‐Earths Exoplanets and Exo‐Mercuries;Journal of Geophysical Research: Planets;2024-06-27
3. Thermal convection and dynamo action with stable stratification at the top of the Earth's outer core;Physics of the Earth and Planetary Interiors;2023-12
4. Effects of the Librationally Induced Flow in Mercury’s Fluid Core with an Outer Stably Stratified Layer;The Planetary Science Journal;2023-09-01
5. A Long-lived Lunar Magnetic Field Powered by Convection in the Core and a Basal Magma Ocean;The Planetary Science Journal;2023-05-01
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