A reappraisal of the Martian36Ar/38Ar ratio

Journal of Geophysical Research: Planets

Volumn 102, Issue E1, 1997, Pages 1653-1661

  Bogard, Donald D ^a  

^a NASA JOHNSON SPACE CENTER   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

ARGON-36/ARGON-38; MARTIAN ATMOSPHERE; MARTIAN METEORITE; NOBLE GAS;

MARS;

EID: 0030746676     PISSN: 01480227     EISSN: None     Source Type: Journal    
DOI: 10.1029/96JE02796     Document Type: Article

References (6)

1. Becker, R.H., and R.O. Pepin, The case for a Martian origin of the shergottites: Nitrogen and noble gases in EETA79001, Earth Planet. Sci. Lett., 69, 225-242, 1984.
2. Becker, R.H., and R.O. Pepin, Nitrogen and noble gases in a glass sample from LEW88516 (abstract), Lunar Planet. Sci., XXIV, 77-78, 1993.
3. 38Ar ratio (abstract), Lunar Planet. Sci., XXVII, 83-84, 1996.
4. Drake, M.J., T.D. Swindle, T. Owen, and D.S. Musselwhite, Fractionated Martian atmosphere in the nakhlites, Meteoritics, 29, 854-859, 1994.
5. Hunten, D.M., R.O. Pepin, and J.G.G. Walker, Mass fractionation in hydrodynamic escape, Icarus. 69, 532-549, 1987.
6. Wiens, R.C., R.H. Becker, and R.O. Pepin, The case for a Martian origin of the shergottites, II, Trapped and indigenous gas components in EETA79001 glass. Earth Planet. Sci. Lett., 77, 149-158, 1986.