TAFASSASSET

Twenty-six stones totaling ~110 kg, the two largest weighing ~30 kg, were found by Bernard Dejonghein in the Ténéré region of north-central Niger; all are considered to be paired. This olivine-rich meteorite was classified at the Muséum National d'Histoire Naturelle in France as the first thermally metamorphosed CR chondrite.

A separate ~3.6 kg stone found independently in the same vicinity as Tafassasset was provisionally named Te-1 (and synonym Grein 004), and it was independently analyzed at the Max-Planck-Institut für Chemie in Germany. A bulk compositional analysis of Te-1 found that it differs slightly from Tafassasset in its texture and in certain hosted elemental abundances, but its overall similarity in texture and elemental composition with Tafassasset makes their pairing obvious; this suggests that this fall was composed of a heterogeneous assemblage. Since the classification of Te-1 preceded that of Tafassasset, the name proposed for this fall may rightly belong to the German team.

Although these stones are only slightly weathered to a grade of W0/1, the majority of the fusion crust has been extensively sand-blasted off. Relict chondrules and chondrule rims in Tafassasset have been reported by the French research team. These chondrule relicts would be most consistent with a porphyritic olivine–pyroxene type; some are metal-bearing. A related anomalous achondrite, RBT 04239, contains relict prophyritic chondrules, some of which are ~1.2 mm in diameter. Tafassasset is consistent with a CR chondrite relationship with respect to its high abundance of siderophile elements, including its high FeNi-metal content of 8–10 vol% compared to ~7.4 vol% in CR chondrites (Nehru et al., 2010).

Plagioclase, chromite, and phosphates present in the matrix of Tafassasset have been attributed to metamorphism of original fine-grained matrix material. In contrast, similar mineral phases are found in areas that define possible relict chondrules, but these phases have retained the textures of an earlier, pre-metamorphic stage. Small, abundant sulfide grains present in the recrystallized olivine-pyroxene matrix within Tafassasset are similar to those found in CR chondrites. The O-isotopes also plot within the CR field and away from the majority of brachinites, with the exception of the anomalous brachinite LEW 88763. Still, the plagioclase composition and other silicate abundances in Tafassasset is most similar to that of the brachinites.

Tafassasset has a fractionated element signature uncharacteristic for the CR group, including a depletion in refractory lithophile elements, an extremely low Zn concentration, and Al/Mg and Mn/Mg ratios that plot near the primitive achondrites. This fractionation is consistent with an early stage of partial melting involving the mobilization of melts incorporating Si, P, and S. Classification as an ungrouped primitive achondrite has been suggested as the most plausible classification by the German research team (Zipfel et al., 2002).

An advanced stage of metamorphism compared to that exhibited by the CR6-like chondrites NWA 2994 and NWA 3100 has been invoked by Bunch et al (2008) to explain the recrystallized poikiloblastic texture in Tafassasset. They also argue that the similarity in O-isotopic compositions which is observed among the nonmetamorphosed CR chondrites, the metamorphosed CR6-like chondrites and Tafassasset, and the igneous achondrite NWA 011 (and pairings), is consistent with their derivation from a common, large parent body, one which experienced internal partial melting while retaining a chondritic regolith.

A study which compared Tafassasset with the brachinites was undertaken by Nehru et al. (2003). They determined that the texture, modal abundances, and mineral compositions of Tafassasset were very similar to Brachina, while some differences were found to exist in its equilibration temperature, O-isotopic composition (though it is similar to the anomalous brachinite LEW 88763), and high metal abundance. In a similar comparison made by Patzer et al. (2003), it was found that the level of radiogenic 129Xe measured in Tafassasset is similar to that of some brachinites. They also found that the trapped 132Xe component of Tafassasset was lower than that of CR chondrites, and that the 36Ar/132Xe ratio is at least 10× lower than it is in CR chondrites. As with brachinites, Tafassasset was determined to have an ancient Pb–Pb age of ~4.563 b.y. (Göpel et al., 2009). They also found that its Cr systematics are the same as they are in Renazzo, and that its excess of 54Cr is the first such occurrence in a non-carbonaceous meteorite (Göpel and Birck, 2010).

Tafassasset (and the paired Te-1) is a primitive achondrite that is petrographically consistent with a low-degree partial melt of Renazzo-like precursor material which has retained its metal component. It subsequently experienced equilibration processes through an extended period of thermal metamorphism. Tafassasset is considered to be closely related to the brachinites and other FeO-rich primitive achondrites, and has been characterized by Nehru et al. (2010) as an unusual brachinite derived from a CR-like precursor body which experienced partial differentiation. A Fa vs. Fs plot demonstrates this genetic relationship, as well as a relationship between the more primitive anomalous achondrites Divnoe and RBT 04239 (Gardner et al., 2007). A close relationship between Tafassasset and the CR group may be excluded based on differences in elemental compositions, noble gas ratios, and solar gas abundances. The CRE age of Tafassasset is also much higher (76.1 ±15.2 m.y.) than that of any CR chondrite (<10 m.y.). However, it has been suggested that all of these differences between Tafassasset and CR chondrites may be the result of the increased degree of metamorphism experienced by Tafassasset.

In a new petrographic analysis and O-isotope study conducted by Gardner-Vandy et al. (2008, LPSC 39, #2307), it was found that their sample of Tafassasset has O-isotopic ratios which plot within the LL-chondrite field and well away from the CR field. In light of these results, they suggest that this meteorite originated on an FeO-rich parent body which formed near the CR-chondrite region and experienced a low degree of melting, without reaching isotopic homogeneity. Further studies are required to definitively satisfy the classification issues surrounding Tafassasset. The specimen of Tafassasset pictured above is a 4.45 g partial slice with an edge of preserved fusion crust.

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