NWA 1465 was first recovered out of the desert in Western Sahara in 2001. Approx. 3 kilograms of fusion crusted stones were found and samples were classified as a shocked CV3 chondrite. It has a wealth of chondrules and CAI inclusions set into a dark fine-grained groundmass. There are also clasts of darker material whose oxygen isotope range measure outside that of the host rock, and thus the official classification is CV3 anomalous. A modest amount of this material made it onto the collector market many years ago and is rarely seen on the market now.
The specimen being offered here is a professionally-prepared endcut that is polished on one side. It weighs 5.84 grams.
Refer to the photos. The black centimeter cube is shown for scale and is not included. You are purchasing the specimen shown. Your purchase will include an ID label and padded box for storage.
From the Meteoritical Bulletin entry for NWA 1465 :
Northwest Africa 1465
Carbonaceous chondrite (CV3 anomalous)
Many pieces totalling 3000 g and mostly covered with fusion crust were found in 2001 by an anonymous finder in the Western Saharan desert. Classification and mineralogy (A. Greshake, MNB and M. Kurz, Kurz): a type 3 carbonaceous chondrite with chondrules, mineral fragments, and refractory objects in a compact anhydrous matrix of Fe-rich olivine, Ca-rich pyroxene, enstatite, forsterite, troilite, magnetite, FeNi-metal, and weathering products; shows a strong foliation defined by flattened chondrules and refractory objects; the sample contains cm-sized Ca,Al-rich inclusions and large inclusions of dark material (Greshake et al., 2003); oxygen isotope composition of the bulk meteorite (R. Clayton and T. Mayeda, UChi) oxygen isotope composition of dark material, not in equilibrium with the host meteorite. Shock stage, S4; degree of weathering, W3. Specimens: type specimen, 21.8 g, and one polished thin section, MNB; main mass with anonymous finder.