We present the first observations of seismic waves propagating through the core of Mars.
These observations, made using seismic data collected by the InSight geophysical mission …

This review summarizes the knowledge of Mars' interior structure, its inferred composition,
and the anticipated seismological properties arising from its composition with particular …

Mantle control on planetary dynamos is often studied by imposing heterogeneous core-
mantle boundary (CMB) heat flux patterns on the outer boundary of numerical dynamo …

Several episodes of complete melting have probably occurred during the first stages of the
Earth's evolution. We have developed a numerical model to monitor the thermal and melt …

The Earth is a thermal engine generating the fundamental processes of geomagnetic field,
plate tectonics and volcanism. Large amounts of heat are permanently lost at the surface …

The evolution and internal structure of Mars are, by comparison to its present-day surface,
poorly known—although evidence of recent volcanic activity suggests that its deep interior …

Meteorites are interpreted as relics of early formed planetary bodies, and they provide
information about the processes that occurred in the first few Myrs of our solar system. The …

We present a thermal evolution model coupled with a Henyey solver to study the
circumstances under which a rocky planet could potentially host a dynamo in its liquid iron …

The MESSENGER mission revealed that Mercury's magnetic field might have operated
since 3.7–3.9 Ga. While the intrinsic magnetism suggests an active dynamo within Mercury's …

Due to mechanisms such as impact heating, early atmospheric thermal blanketing, and
radioactive heating, the presence of at least one global magma ocean stage in the early …