The dynamics and evolution of Venus' mantle are of first-order relevance for the origin and
modification of the tectonic and volcanic structures we observe on Venus today. Solid-state …

Plate tectonics is a particular mode of tectonic activity that characterizes the present-day
Earth. It is directly linked to not only tectonic deformation but also magmatic/volcanic activity …

Cratons record the early history of continental lithosphere formation, yet how they became
the most enduring part of the lithosphere on Earth remains unknown. Here we propose a …

The thermal and chemical evolution of rocky planets is controlled by their surface tectonics
and magmatic processes. On Earth, magmatism is dominated by plutonism/intrusion versus …

Thermomechanical models of mantle convection and melting in an inferred hotter Archean
Earth show the emergence of pressure-temperature (PT) regimes that resemble present-day …

The processes that operated on the early Earth and the tectonic regimes in which it was
shaped are poorly constrained, reflecting the highly fragmentary rock record and uncertainty …

The crust-mantle dynamic system of the formation and evolution of the early Earth crust is a
frontier field in current Earth Science. This paper mainly introduces the popular dynamic …

Following our recent investigation [G. Kefayati,“Internally heated convection of viscoplastic
fluids in enclosures using a lattice Boltzmann method,” Phys. Fluids 35, 013108 (2023)], this …

A nearly pole‐to‐pole survey near 140° E longitude on Europa revealed many areas that
exhibit past lateral surface motions, and these areas were examined to determine whether …

As the Earth's primary mode of planetary cooling, the oceanic plate is created at mid-ocean
ridges, transported across the planet's surface, and destroyed at subduction zones. The …