Geology Reference
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Quantifying noble gas contamination during terrestrial
alteration in martian meteorites from Antarctica,
Meteorit. Planet. Sci. , 48 , 929-954.
[779] Shearer, C. K., P. V. Burger, J. J. Papike , L. E. Borg, A. J.
irving, and C. Herd (2008), Petrogenetic linkages among
martain basalts: implications based on trace element chem-
istry of olivine, Meteorit. Planet. Sci. , 43 , 1241-1258.
[780] Shih, C.-y., L. A. Nyquist, and y. Reese (2009), Rb-Sr
and Sm-Nd studies of olivine-pyric Shergotties RBT 04262
and LAR 06319: isotopic evidence for relationship to
enriched basaltic shergottites, Lunar Planet. Sci. , 40 ,
abstract 1360.
[781] Usui, T., M. E. Sanborn, M. Wadhwa, and H. y. McSween
(2010), Petrology and trace element geochemistry of
Robert Massif 04261 and 04262 meteorites, the first
examples of geochemically enriched lherzolitic shergot-
tites, Geochim. Cosmochim. Acta , 74 , 7283-7306.
[791] imae, N., and y. ikeda (2008), Crystallization experi-
ments of intercumulus melts for nakhlites under QFM
±2 at 1 bar, Meteorit. Planet. Sci. , 43 , 1299-1319.
[792] Kuebler, K. E. (2013), A combined electron microprobe
(EMP), and Raman spectroscopic study of the alteration
products in martian meteorite MiL 03346, J. Geophys.
Res. , 118 , 347-368.
[793] McCubbin, F. M., N. J. Tosca, A. Smirnov, H. Nekvasil,
A. Steele, M. Fries, and D. H. Lindsley (2009),
Hydrothermal jarosite and hematite in a pyroxene-
hosted melt inclusion in martian meteorite Miller Range
(MiL), 03346: implications for magmatic-hydrothermal
fluids on Mars, Geochim. Cosmochim. Acta ,
73 ,
4907-4917.
[794] Mikouchi, T., A. Monkawa, E. Koizumi, J. Chokai, and
M. Miyamoto (2005), MiL 03346 nakhlite and NWA2737
“Diderot” chassignite: Two new martian cumulate rocks
from hot and cold deserts, Lunar Planet. Sci. Conf. 36 ,
abstract 1944.
[795] Mikouchi, T., M. Miyamoto, E. Koizumi, J. Makishima,
and g. McKay (2006), Relative burial depths of nakhlites:
An update, Lunar Planet. Sci. Conf. , 37 , abstract 1865.
[796] Park, J., D. H. garrison, and D. D. Bogard (2009),
39 Ar- 40 Ar ages of martian nakhlites, Geochim. Cosmochim.
Acta , 73 , 2177-2189.
[797] Righter, K., and K. M. McBride (2012), The Miller
Range nakhlites: A summary of the curatorial subdivi-
sion of the main mass in light of newly found paired
masses, Lunar Planet. Sci. Conf. , 42 , LPi Contribution
No. 1608, 2161.
[798] Righter, K., H. yang., g. Costin., and R. T. Downs
(2008), oxygen fugacity in the martian mantle controlled
by carbon: New constraints from the nakhlite MiL
03346, Meteorit. Planet. Sci. , 43 , 1709-1723.
[799] Rutherford, M. J., and J. E. Hammer (2008), oxidation
states in MiL 03346 nakhlite from experiments reproduc-
ing phenocryst-melt equilibria as a function of fo 2 and
T  at 40-150 Mpa, Lunar Planet. Sci. Conf. , 39 , LPi
Contribution No. 1391, 1983.
[800] Rutherford, M. J., C. Calvin, M. Nicholis, and M. C.
McCanta (2005), Petrology and melt compositions in
nakhlite MiL 00346: Significance of data from natural
sample and from experimentally fused groundmass and
M.i.'s, Lunar Planet. Sci. Conf. , 36 , abstract 2233.
[801] Sautter, V., A. Jambon, and o. Boudouma (2006),
Cl-amphibole in the nakhlite MiL03346: Evidence for
sediment contamination in a martian meteorite, Earth
Planet . Sci. Lett. , 252 , 45-55.
[802] Stopar, J. D., g. J. Taylor, M. A. Velbel, M. D. Norman,
E. P. Vicenzi, and L. J. Hallis (2013), Element abundances,
patterns, and mobility in Nakhlite Miller Range 03346
and implications for aqueous alteration, Geochim.
Cosmochim. Acta , 112 , 208-225.
[803] Udry, A., H. y. McSween, Jr., P. Lecumberri-Sanchez, R.
J. Bodnar (2012), Paired nakhlites MiL 090030, 090032,
090136, and 03346: insights into the Miller Range parent
meteorite, Meteorit. Planet. Sci., 47 , 1575-1589.
74. MiL 03346—NAKHLiTE
[782] Cartwright, J. A., J. D. gilmour, and R. Burgess (2013),
Martian fluid and martian weathering signatures identified
in Nakhla, NWA 998 and MiL 03346 by halogen and noble
gas analysis, Geochim. Cosmochim. Acta , 105 , 255-293.
[783] Day, J. M. D., L. A. Taylor, C. Floss, and H. y. McSween
(2006), Petrology and chemistry of MiL 03346 and its
significance in understanding the petrogenesis of
nakhlites on Mars, Meteoritics , 40 , 581-606.
[784] Debaille, V., A. D. Brandon, C. o'Neill, Q.-Z. yin, and B.
Jacobsen (2009), Early martian mantle overturn inferred
from isotopic composition of nakhlite meteorites, Nature
Geoscience , 2 , 548-552.
[785] Dyar, M. D., A. H. Treiman, C. M. Pieters, T. Hiroi, M.
D. Lane, and V. o'Connor (2005), MiL03346, the most
oxidized martian meteorite: A first look at spectroscopy,
petrography, and mineral chemistry, J. Geophys. Res. ,
110 , E09005.
[786] 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.
[787] Hallis, L. J., g. J.Taylor, K. Nagashima, g. R. Huss, A.
W. Needham, M. M.grady, and i. A. Franchi (2012),
Hydrogen isotope analyses of alteration phases in the
nakhlite martian meteorites, Geochim. Cosmochim. Acta ,
97 , 105-119.
[788] Hallis, L. J. (2013), Alteration assemblages in the Miller
Range and Elephant Moraine regions of Antarctica:
Comparisons between terrestrial igneous rocks and mete-
orites, Meteorit. Planet. Sci. 48 , 165-179.
[789] Hammer, J. E. (2009), Application of a textural geospeed-
ometer to the late-stage magmatic history of MiL 03346,
Meteorit. Planet. Sci. , 44 , 141-154.
[790] imae, N., and y. ikeda (2007), Petrology of the Miller Range
03346 nakhlite in comparison with the yamoto-000593
nakhlite, Meteorit. Planet. Sci. , 42 , 171-184.
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