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
The adjoint equations for thermochemical compressible mantle convection: derivation and verification by twin experiments. [PDF]
Ghelichkhan S, Bunge HP.
europepmc +1 more source
Continuous reorientation of synchronous terrestrial planets due to mantle convection. [PDF]
Leconte J.
europepmc +1 more source
The assumption that stationary hotspots underlie the Earth’s lithospheric plates has been most important in the development of the theory of plate tectonics. According to the fixed hotspot hypothesis seamount trails are formed by volcanism penetrating the
Antretter, Maria
core
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
Understanding magma genesis through analysis of melt inclusions: application of innovative micro-sampling techniques [PDF]
Melt entrapped as inclusions in early-formed phenocrysts provide geochemists with an exceptional opportunity to study sample material from the earliest stages in the formation of a suite of lavas.
Harlou, Rikke
core
A rapid tectonic plate reorganization event driven by changes at subduction locations in a mantle convection model. [PDF]
Guerrero JM +4 more
europepmc +1 more source
Effect of bridgmanite-ferropericlase grain size evolution on Earth's average mantle viscosity: implications for mantle convection in early and present-day Earth. [PDF]
Paul J +5 more
europepmc +1 more source

