(ungrouped achondrite in MetBull 91)
Found June 2006
no coordinates recorded
A fresh, fusion-crusted, 625 g stone was found in the Algerian desert in June of 2006; shortly thereafter it was purchased by a collector (A. Aaronson) in Erfoud, Morocco, and a portion of the meteorite was submitted for analysis and classification to Northern Arizona University (T. Bunch and J. Wittke) and the University of Washington in Seattle (A. Irving). The meteorite was subsequently sold to another collector (S. Turecki). The section of NWA 2993 under analysis was found to consist of 37 vol% orthopyroxene, 32 vol% olivine, and 30 vol% FeNi-metal (kamacite-rimmed taenite with occasional plessite cores), along with minor sulfide.
While a preliminary petrographic examination of a cut face revealed the texture and composition of a coarse-grained (0.33.4 mm), plagioclase-depleted, metal-rich lodranite, subsequent O-isotopic analyses conducted at Carnegie Institute (D. Rumble, III) showed that it actually plots on an extension of the trend line for the winonaite/IAB-iron complex meteorites; it is also notable that NWA 2993 plots very close to the pyroxene pallasite Vermillion (see Figure 3 in the 38th LPSC abstract #2211 ). To help discriminate between the winonaite and acapulcoitelodranite groups, a plot of Δ17O () with olivine Fa content (mol%) was found to be a useful technique (D. Rumble, III et al., 2005). Northwest Africa 2993 plots nearest to the winonaite field, but since it has the largest values for both parameters, it plots in a unique location slightly distant from the main winonaite concentration (see Figure 4 in abstract #2211 above).
*Previously, Floss (2000) and Patzer et al. (2003) proposed that the acapulcoite/lodranite meteorites should be divided based on metamorphic stage:
primitive acapulcoites: near-chondritic (Se >1213 ppm [degree of sulfide extraction])
typical acapulcoites: FeNiFeS melting and some loss of sulfide (Se ~512 ppm)
transitional acapulcoites: sulfide depletion and some loss of plagioclase (Se <5 ppm)
lodranites: sulfide, metal, and plagioclase depletion (K <200 ppm [degree of plagioclase extraction])
enriched acapulcoites (addition of feldspar-rich melt component)
A similar distinction could be made among the winonaites in our collections, although there is not yet an analog of the IAB complex irons for the acapulcoite/lodranite PB. Northwest Africa 1463 (and pairing group) ranks as the most primitive member of the winonaites, containing intact chondrules comparable to a petrologic type 5 chondrite (Benedix et al., 2003). However, most winonaites experienced extensive thermal metamorphism involving incipient sulfide melting and exhibit highly recrystallized textures, characteristics analogous to the "typical" acapulcoites. Metamorphic progression in other winonaites led to partial loss of the low-melting phases FeS and plagioclase, and these are designated as a "transitional" stage in the acapulcoite/lodranite metamorphic continuum. Those winonaites which experienced the highest temperatures ultimately crystallized from residual melt material, and they exhibit significant depletions in FeS, FeNi-metal, and plagioclase (including plagiophile trace elements). Samples representing this advanced metamorphic stage are known as lodranites in the acapulcoite/lodranite metamorphic sequence, while the term "evolved" could be used to represent a similar metamorphic stage in the winonaite group (e.g., Tierra Blanca; Hunt et al., 2017).
Northwest Africa 2993 represents the first known coarse-grained, plutonic sampling from the winonaite/IAB-iron complex parent body, and is chemically and texturally analogous to the lodranites of the ACALOD parent body. Determination of the exact petrogenetic history which led to the formation of this unique meteorite is ongoing, and further details about the winonaite group can be found on the Tierra Blanca page. The photo of NWA 2993 shown above is a 8.93 g slice, while that below is a view of the main mass in the possession of the owner.