Kainsaz Meteorite
History
A fireball was observed which left a dust train and broke into fragments during flight in a series of detonations that were heard up to 130 kilometres (81 mi) away. The strewn field of 40 by 7 kilometres (24.9 mi × 4.3 mi) was oriented SE-NW with the largest stone falling at the NW end, the smallest (the size of a nut) near the village of Kosteevo at the SE end.
Mineralogy
Most of the chondrules (90 %) are either droplet (39 %) or lithic (61 %). The remaining 10 % are barred olivine, radial pyroxene, cryptocrystalline, glassy, sulfide-metal, micro-poikilitic and complex chondrules.
Classification
Kainsaz is classified as a CO3.2. This stands for CO group, petrologic type = 3, and subtype = 2. The group is part of the CM-CO clan and a member of the carbonaceous chondrites.
See also
References
- ^ Millman, P. M. (Oct–Dec 1938). "News from the Soviet Union Concerning Meteoric Research". Journal of the Royal Astronomical Society of Canada. 33: 51. Retrieved 11 January 2013.
- ^ "Kainsaz CO3.2 Carbonaceous Chondrite Meteorites for Sale". The Meteorite Market. Retrieved 11 January 2013.
- ^ "Kainsaz". Meteoritical Bulletin Database. Meteoritical Society. Retrieved 11 January 2013.
- ^ Stakheeva, S. A. "Chondrules in the Kainsaz CO chondrite" (PDF). Retrieved 12 January 2013.