The case for planetary sample return missions: 1. Origin of the solar system

Eos, Transactions American Geophysical Union

Volumn 68, Issue 8, 1987, Pages 105-113

  Drake, Michael J ^a   Boynton, William V ^a   Blanchard, Douglas P ^b  

^a UNIVERSITY OF ARIZONA   (United States)

^b NASA JOHNSON SPACE CENTER   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 84984515150     PISSN: 00963941     EISSN: 23249250     Source Type: Journal    
DOI: 10.1029/EO068i008p00105-02     Document Type: Article

References (17)

1. Martian gases in an Antarctic meteorite?
2. Composition and evolution of the eucrite parent body: Evidence from rare earth elements
3. Siderophile elements in planetary mantles and the origin of the moon
4. Rotational spectral variations of Asteroid (8) Flora: Implications for the nature of the S‐type asteroids and for the parent bodies of the ordinary chondrites
5. Compositional structure of the asteroid belt
6. Planetesimals to planets: Numerical simulation of collisional evolution
7. Geochemical constraints on core formation in the earth
8. Chemical systematics of the Shergotty meteorite and the composition of its parent body (Mars)
9. SNC meteorites: Clues to Martian petrologic evolution?
10. Core formation in the earth and shergottite parent body (SPB): Chemical evidence from basalts
11. Constitution of the terrestrial planets
12. Occurrence of giant impacts during the growth of the terrestrial planets