Solar wind origin of 36Ar on Venus

Icarus

Volumn 46, Issue 1, 1981, Pages 70-80

  Wetherill, George W ^a  

^a GEOPHYSICAL LABORATORY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0002507382     PISSN: 00191035     EISSN: 10902643     Source Type: Journal    
DOI: 10.1016/0019-1035(81)90076-2     Document Type: Article

References (38)

1. 87Sr method
2. The primitive solar accretion disk and the formation of the planets
3. Terrestrial abundance of noble gases
4. Asteroids as meteorite parent-bodies: The astronomical perspective
5. Primordial noble gases in E-chondrites
6. Primordial neon, helium, and hydrogen in oceanic basalts
7. Physical adsorption of rare gas on terrigeous sediments
8. Numerical simulation of planet growth: Early runaway growth
9. Planetesimals to planets: Numerical simulation of collisional evolution
10. Long-term behavior of planetesimals and the formation of planets
11. Primordial metamorphism of asteroids via electrical induction in a T Tauri-like solar wind
12. Composition of the Venus lower atmosphere from the Pioneer Venus mass spectrometer
13. Cosmogony of the solar system
14. Dynamics of lunar origin and orbital evolution
15. Distribution properties of implanted rare gases in individual olivine crystals from the lunar regolith
16. Growth of solid particles in the primordial solar nebula
17. SmNd ages: A new dating method
18. Xenon in carbonaceous shondrites
19. Upper limits on argon isotope abundances in the Venus thermosphere
20. Noble gases in carbonaceous chondrites
21. Dissolution of the primordial rare gases into the molten Earth's material
22. Implitations of the gas compositional measurements of Pioneer Venus for the origin of planetary atmosphere
23. Dissipation of the rare gases contained in the primordial Earth's atmosphere
24. Implications of argon-36 excess on Venus
25. The melting of asteroidal-sized bodies by unipolar dynamo induction form a primordial T Tauri sun
26. Noble gases in separated meteorite minerals Murchison (C2) Ornans (C3) Karoonda (C5) and Abee (E4)
27. The cosmic abundances of potassium uranium and thorium and the heat balances of the Earth Moon and Mars
28. Late heavy bombardment of the moon and terrestrial planets
29. Evolution of the Earth's planetesimal swarm subsequent to the formation of the earth and moon
30. Accumulation of the terrestrial planets
31. Formation of the terrestrial planets
32. Numerical calculations relevant to the accumulation of the terrestrial planets
33. 36Ar in the atmosphere of the Venus?
34. Origin of differentiated meteorites
35. Radial pressure in the solar nebula as affecting the motions of planetesimals