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"Abstract: A garnet-bearing clast has been identified in martian breccia meteorite NWA 8171, comprising two distinct domains: an andradite-diopside domain, and a K-feldspar-augite domain. Similar assemblages occur in terrestrial metamorphic/metasomatic settings like skarns, in alkali igneous rocks; and as secondary phases in carbonaceous chondrites. Mineralogical and textural analyses of the clast reveals a complex history, possibly reflecting multiple crystallisation stages and/or alteration events on Mars. However, as NWA 8171 is a regolith breccia, we also consider if the garnet-bearing clast is extra-martian in origin. Analysis of pyroxene Mn/Fe ratios indicate that augites from the K-feldspar-rich domain match martian values, while diopsides in the andradite-bearing domain are more varied in composition. This variability, together with similarities to metasomatic assemblages from chondritic and terrestrial analogues, suggests that the andradite-rich domain may not comprise primary igneous minerals. This could indicate the clast was altered on Mars in an oxidising metasomatic event, although an extra-martian origin cannot be ruled out. Still, the first identification of garnet in a martian meteorite has major implications. The andradite-bearing clast in NWA 8171 may be the first sample of a garnet-bearing lithology from Mars, representing a previously unidentified martian magma source, alteration process, regolith impactor component, or metamorphic event."
"T.V. Kizovski, L.F. White, A. ÄŒernok, K.T. Tait, V.E. Di Cecco, X. Chu, J.M. Tomacic, R.I. Nicklin, J.R. Darling"
"Geochem. Persp. Let. (2026) 40, 30–37 | doi: 10.7185/geochemlet.2619 | Published 16 June 2026"