The article is missing a description of the genesis of the asteroidal material. Almahata Sitta is a ureilite (among other things), which cooled from very high temperatures (in excess of 1100C) during its formation.
-- Mark --- On Thu, 12/30/10, Matson, Robert D. <[email protected]> wrote: > So something must be missing from the article to explain > why they > believe Almahata Sitta's interior got so hot. [snip] > So the question is, am I missing something? --Rob ______________________________________________ Visit the Archives at http://www.meteoritecentral.com/mailing-list-archives.html Meteorite-list mailing list [email protected] http://six.pairlist.net/mailman/listinfo/meteorite-list
