Geology Reference
In-Depth Information
These meteorites have provided a record of martian
magmatic activity extending from Noachian time to
nearly the present. In addition, their secondary minerals
serve as physical witnesses to martian history and provide
critical insight into the dramatic climate changes Mars has
experienced. The ability to analyze their geochemistry,
radiometric ages, and petrology complements and extends
what has been learned from spacecraft exploration, and
helps to make Mars the most completely studied extrater-
restrial body.
Bradley, J. P., H. Y. McSween Jr., and R. P. Harvey (1998),
Epitaxial growth of nanophase magnetite in martian meteorite
Allan Hills 84001: Implications for biogenic mineralization,
Meteorit. Planet. Sci ., 33 , 765-773.
Brearley, A. (2003), Magnetite in ALH 84001: An origin by
shock-induced thermal decomposition of iron carbonate,
Meteorit. Planet. Sci ., 38 , 849-870.
Bridges, J. C., and P. H. Warren (2006), The SNC meteorites:
Basaltic igneous processes on Mars, J. Geol. Soc. London ,
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Clement, S. J., and R. N. Zare (1996), Response to technical
comment, Science , 274 , 2122-2123.
Corrigan, C. M., and R. P. Harvey (2004), Multi-generational
carbonate assemblages in martian meteorite Allan Hills
84001: Implications for nucleation, growth, and alteration,
Meteorit. Planet. Sci ., 39 , 17-30.
Day, J. M. D., L. A. Taylor, C. Floss, and H. Y. McSween
Jr.  (2006), Petrology and chemistry of MIL 03346 and its
significance in understanding the petrogenesis of nakhlites
on Mars, Meteorit. Planet. Sci ., 41 , 581-606.
Dyar, M. D., A. H. Treiman, C. M. Pieters, T. Hiroi, M. D. Lane,
and v. O'Connor (2005), MIL 03346, the most oxidized mar-
tian meteorite: A first look at spectroscopy, petrography, and
mineral chemistry, J. Geophys. Res., 110 , E09005, 2005JE00246.
Eiler, J. M., J. W. valley, C. M. Graham, and J. Fournelle (2002),
Two populations of carbonate in ALH 84001: Geochemical
evidence for discrimination and genesis, Geochim. Cosmochim.
Acta , 66 , 1285-1303.
Gibson, E. K., D. S. McKay, K. L. Thomas-Keprta,
S.  J.  Wentworth, F. Westall, A. Steele, C. S. Romanek,
M. S. Bell, and J. Toporski (2001), Life on Mars: Evaluation
of the evidence within martian meteorites ALH84001,
Nakhla, and Shergotty, Precambrian Res ., 106 , 15-34.
Golden, D. C., H. v. Lauer, G. E. Lofgren, G. A. McKay,
D. W. Ming, R. v. Morris, C. S. Schwandt, and R. A. Socki
(2001), A simple inorganic process for formation of carbonates,
magnetite, and sulfides in martian meteorite ALH 84001, Amer.
Mineral ., 86 , 370-375.
Goodrich, C. A. (2003), Petrogenesis of olivine-phyric
shergottites Sayh al Uhaymir 005 and Elephant Moraine
A79001 lithology A, Geochim. Cosmochim. Acta , 67 ,
3735-3771.
Goodrich, C. A., C. D. K. Herd, and L. A. Taylor (2003),
Spinels and oxygen fugacity in olivine-phyric and lherzolitic
shergottites, Meteorit. Planet. Sci ., 38 , 1773-1792.
Greenwood, J. P., and H. Y. McSween Jr. (2001), Petrogenesis
of Allan Hills 84001: Constraints from impact-melted
feldspathic and silica glasses, Meteorit. Planet. Sci ., 36 ,
43-61.
Hallis, L. J., and G. J. Taylor (2011), Comparisons of the four
Miller Range nakhlites, MIL 03346, 090030, 090032 and
090136: Textural and compositional observations of primary
and secondary mineral assemblages, Meteorit. Planet. Sci .,
46 , 1787-1803.
Harvey, R. P., and v. E. Hamilton (2006), Syrtis Major as the
source region of the nakhlite/Chassigny martian meteorites
(abstract), Meteorit. Planet. Sci ., 40 , A65.
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