Signatures of early differentiation of Mars

Earth and Planetary Science Letters

Volumn 196, Issue 3-4, 2002, Pages 251-263

  Marty, Bernard ^a,b,c   Marti, Kurt ^a  

^a UNIVERSITY OF CALIFORNIA   (United States)

^b CRPG CNRS   (France)

^c UNIVERSITÉ DE LORRAINE   (France)

Author keywords

Mars; Pu 224; Radioactivity; Xenon

Indexed keywords

ISOTOPIC FRACTIONATION; MARS; PLANETARY EVOLUTION; PLUTONIUM; RADIOACTIVITY; XENON;

EID: 0036261309     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0012-821X(01)00612-4     Document Type: Article

References (53)

1. The accretion, composition and early differentiation of Mars
2. The age of the Earth
3. Rapid accretion and early differentiation of Mars indicated by Nd-142 Nd-144 in SNC meteorites
4. Core formation on Mars and differentiated asteroids
5. On the origin and early evoluation of terrestrial planetary atmospheres and meteoritic volatiles
6. Evolution of the Martian atmosphere
7. An outgassing release factor for non-radiogenic volatiles on Mars
8. How many Martian noble gas reservoirs have we sampled?
9. The composition of the atmosphere at the surface of Mars
10. Martian gases in an Antarctic meteorite
11. Signatures of the Martian atmosphere in glass of the Zagami meteorite
12. Early out-gassing of Mars supported by differential water solubility of iodine and xenon
13. Early outgassing of Mars: Implications from experimentally determined solubility of iodine in silicate magmas
14. Chronology and evolution of Mars
15. Early evolution of Martian volatiles: Nitrogen and noble gas components in ALH84001 and Chassigny
16. Martian atmospheric and interior volatiles in the SNC meteorite Nakhla
17. Martian interior volatiles: Indigenous signatures and early evolution
18. Volatiles on Earth and Mars - A comparison
19. Magma generation on Mars - Amounts, rates, and comparisons with Earth, Moon, and Venus
20. Rare gas systematics in Popping Rock: Isotopic and elemental compositions in the upper mantle
21. Abundances of the elements: Meteoritic and solar
22. Characterization of Q-gases and other noble gas components in the Murchison meteorite
23. Active capture of volatiles: Implications for planetary and atmospheric xenon
24. Origin of planetary primordial rare gas: The possible role of adsorption
25. Noble gas trapping by laboratory carbon condensates
26. Comets, impacts, and atmospheres
27. Comets, meteorites and atmospheres
28. Composition of the Earth's upper mantle - I: Sidercphile elements in ultramafic nodules
29. Core growth and siderophile element depletion of the mantle during homogeneous Earth accretion
30. Re-Os isotopic evidence for early differentiation of the Martian mantle
31. Metal/silicate equilibrium in an homogeneous accreting Earth: New results for Re
32. Nd isotopic systematics of Chassigny
33. Isotopic constraints on differentiation and evolution of SNC meteorites
34. Origin and evolution of the Nakhla meteorite inferred from Sm-Nd and U-Pb systematics and REE, Ba, Sr, Rb abundances
35. Sm-Nd-Pu timepieces in the Angra Dos Reis meteorite
36. 244Pu as inferred from the St Severin chondrite
37. ALH84001: Alien or progenitor of the SNC family?
38. 'Martians' young and old: Zagami and ALH84001
39. Cosmic-ray and gas-retention ages of Chassigny meteorite
40. 40Ar chronology of related achondrites
41. Martian atmospheric xenon contents of Nakhla mineral separates: Implications for the origin of elemental mass fractionation
42. The Lu-Hf isotope geochemistry of shergottites and the evolution of the Martian mantle-crust system
43. Constraints on rare gas partition coefficients from analysis of olivine-glass from a picritic mid-ocean ridge basalt
44. Noble gases as trace elements in magmatic processes
45. Chemical composition and accretion history of terrestrial planets
46. 3He in deep waters on the East Pacific Rise
47. Ar isotopes and Earth-atmosphere evolution models
48. Upper mantle origin for Harding County well gases
49. Primordial noble gases from the Earth's mantle identification of a primitive volatile component
50. Impact erosion of the primordial atmosphere of Mars