CHARACTERISTICS OF MARTIAN CRUSTAL MATERIALS AND IMPLICATIONS FOR MAGMATIC
ASSIMILATION: PRELIMINARY Re-Os ISOTOPE AND HIGHLY SIDEROPHILE ELEMENT
ABUNDANCE DATA FOR NAKHLITES AND TISSINT
N. Mari1, A. J. V. Riches2, L. J. Hallis1, M. R. Lee1 1School of Geographical and Earth Sciences, University of
Glasgow, UK. Email: firstname.lastname@example.org 2Department of Earth Sciences, Durham University, UK.
Introduction: Highly siderophile elements (HSE: Re, Au, Os, Ir, Ru, Pt, Rh, and Pd) are particularly important
in constraining planetary formation and evolution processes  and they exhibit chalcophile element behaviour in
the absence of metals, preferring to partition into sulphides [2 and references therein]. Rhenium-osmium isotope
data for the nakhlite martian meteorites are currently limited to only a single analysis of Nakhla . A recent S-
isotope study by Franz et al.  suggested that the nakhlites are affected by variable degrees/types of crustal assimi-
lation, hence Nakhla may not be a reliable indicator of the Re-Os isotope composition of the nakhlite parental mag-
ma. Our project, for the first time, aims to integrate nakhlite Os-isotope compositions and HSE abundance data with
S-isotope compositions for sample fractions for which textural information is constrained prior to destructive anal-
yses. These new data will place valuable constraints on the composition of martian parental melts and the nature of
assimilation/contamination processes involved in nakhlite magma genesis.
The shergottite Tissint was included in our work to test if there is a measureable difference in the Re-Os isotope
and HSE systematics of the nakhlite group and this shergottite - hypothesised to have assimilated crustal sulphur .
Novel methodologies: To precisely and accurately measure HSE abundances and Re-Os isotope compositions in
nakhlite samples we studied two 250 mg chips of both Nakhla and Lafayette, for which textural information was
constrained prior to analyses (Fig. 1). The University of Glasgow ZEISS field-emission SEM within the the Imaging
Spectroscopy and Analysis Centre (ISAAC) was used for textural analyses. Each chip was cut and roughly dry-
polished on one side to allow for SEM X-ray imaging. We also studied multiple saw-cut fractions of Tissint to con-
strain its textural characteristics and their variance prior to destructive analyses. We will utilize ultra-low–blank,
isotope-dilution techniques for HSE and Re-Os isotope analyses at the University of Durham, which are suited to
studies of small sample quantities with low blank/sample ratios and efficient HSE separation.
Fig. 1 - X-ray elemental maps used to retain information on textural characterization of some of our nakhlites
prior to destructive isotopic analyses. (a) Si, Mg, Fe, Ca map of Lafayette, showing abundant cumulus
clinopyroxene (red-orange areas) and minor Fe-rich olivine (green areas); (b) Si, Mg, Fe, Ca map of Nakhla shows
that augite (areas slightly more Mg-rich than Lafayette) and Fe-rich olivine (green areas) are the dominant phases. It
is also possible to see a large sulphate (in dark red, upper right) that we interpret to result from martian crustal
Future work: We will expand and present new nakhlite Re-Os datasets to include the Miller Range nakhlites.
These samples, relative to Lafayette, plot at an extreme of the S-isotope compositional range reported for this mete-
orite group. These data will complement that for Nakhla, which has a S-isotope composition intermediate to that of
the other samples. These new data will constrain how Re-Os isotope compositions and HSE-abundances are affected
by crustal assimilation and will advance our understanding of the derivation of nakhlite parental magmas.
References:  Shirey S. B. and Walker R. J. (1998) Annu. Rev. Earth Planet. Sci. 26:423-500.  Day J. M. D.
et al. (2016) Reviews in Mineralogy & Geochemistry 81:161-238.  Brandon et al. (2000) Geochimica & Cosmo-
chimica Acta 64:4083-4095.  Franz et al. (2014) Nature 508:364-368.  Gattacceca J. et al. (2013) Meteoritics
& Planetary Science 48:1919-1936.
6128.pdf80th Annual Meeting of the Meteoritical Society 2017 (LPI Contrib. No. 1987)