In this chapter, we review the contribution of space missions to the determination of the elemental and isotopic composition of Earth, Moon and the terrestrial planets, with special emphasis on currently planned and future missions. We show how these missions are going to significantly contribute to, or sometimes revolutionise, our understanding of planetary evolution, from formation to the possible emergence of life. We start with the Earth, which is a unique habitable body with actual life, and that is strongly related to its atmosphere. The new wave of missions to the Moon is then reviewed, which are going to study its formation history, the structure and dynamics of its tenuous exosphere and the interaction of the Moon’s surface and exo...
The evolution of planets is driven by the composition, structure, and thermal state of their interna...
Initial and present volatile inventories and distributions in the Earth, other planets, meteorites, ...
The Earth formed over tens of millions of years from an unknown number of stochastic collisions with...
In this chapter, we review the contribution of space missions to the determination of the elemental ...
International audienceIn this chapter we review the contribution of space missions to the determinat...
The composition the atmosphere of Venus results from the integration of many processes entering into...
We review the origin and evolution of the atmospheres of Earth, Venus and Mars from the time when th...
Spacecraft and groundbased observations of the atmospheres of solar system objects have provided a d...
Precise measurements of the chemical, elemental, and isotopic composition of planetary surface mater...
We review the current state of knowledge of the origin and early evolution of the three largest terr...
This paper reviews habitability conditions for a terrestrial planet from the point of view of geosci...
The goal of this session is to use what we understand about other planets and moons in our Solar Sys...
What allows a planet to be both within a potentially habitable zone and sustain habitability over lo...
This thesis is constructed around two distinct topics. The first is the formation history of the Ear...
The terrestrial planetary bodies, the Earth, Moon, Mercury, Venus and Mars, provide geologic records...
The evolution of planets is driven by the composition, structure, and thermal state of their interna...
Initial and present volatile inventories and distributions in the Earth, other planets, meteorites, ...
The Earth formed over tens of millions of years from an unknown number of stochastic collisions with...
In this chapter, we review the contribution of space missions to the determination of the elemental ...
International audienceIn this chapter we review the contribution of space missions to the determinat...
The composition the atmosphere of Venus results from the integration of many processes entering into...
We review the origin and evolution of the atmospheres of Earth, Venus and Mars from the time when th...
Spacecraft and groundbased observations of the atmospheres of solar system objects have provided a d...
Precise measurements of the chemical, elemental, and isotopic composition of planetary surface mater...
We review the current state of knowledge of the origin and early evolution of the three largest terr...
This paper reviews habitability conditions for a terrestrial planet from the point of view of geosci...
The goal of this session is to use what we understand about other planets and moons in our Solar Sys...
What allows a planet to be both within a potentially habitable zone and sustain habitability over lo...
This thesis is constructed around two distinct topics. The first is the formation history of the Ear...
The terrestrial planetary bodies, the Earth, Moon, Mercury, Venus and Mars, provide geologic records...
The evolution of planets is driven by the composition, structure, and thermal state of their interna...
Initial and present volatile inventories and distributions in the Earth, other planets, meteorites, ...
The Earth formed over tens of millions of years from an unknown number of stochastic collisions with...