Results 101 to 110 of about 4,195 (236)
Martian Dichotomy from a Giant Impact: Mantle Convection Models
Kar Wai Cheng +4 more
openalex +1 more source
Energetics of mantle convection and the fate of fossil heat [PDF]
Jun Korenaga
openalex +1 more source
Accelerating the Discovery of Steady‐States of Planetary Interior Dynamics With Machine Learning
Simulating mantle convection often requires reaching a computationally expensive steady‐state, crucial for deriving scaling laws for thermal and dynamical flow properties and benchmarking numerical solutions.
Siddhant Agarwal +4 more
doaj +1 more source
Polar Motion Dynamics on Slow‐Rotating Venus: Signatures of Mantle Flow
With its 1 day lasting 243 days on Earth, Venus is the slowest‐spinning planet in the Solar System and its rotational bulge is anomalously small. A rotational bulge stabilizes the orientation of planets. Having only a tiny stabilizer, the rotational pole
Vojtěch Patočka +2 more
doaj +1 more source
CHARACTERIZATION OF SECONDARY MANTLE CONVECTION FROM GEOPHYSICAL DATA AND MODELS
Claudia Adam, Bimal Pandit
openalex +2 more sources
The adjoint equations for thermochemical compressible mantle convection: derivation and verification by twin experiments. [PDF]
Ghelichkhan S, Bunge HP.
europepmc +1 more source
Sluggish thermochemical basal mantle structures support their long-lived stability
Large low shear-wave velocity provinces (LLSVPs) in the lowermost mantle are the largest geological structures on Earth, but their origin and age remain highly enigmatic.
Zhidong Shi +8 more
doaj +1 more source
Edge-Driven Convection and Mantle Wind Models Beneath Madagascar
Jiashun Hu +5 more
openalex +1 more source
Is a whole-mantle convection the key to solving the Tunguska 1908 problem?
B. R. German
openalex +1 more source

