[meteorite-list] Patterns in Sikhote-Alin
From: meteoriteshow <meteoriteshow_at_meteoritecentral.com>
Date: Thu Apr 22 10:17:48 2004 Message-ID: <00e901c3c3c8$19af4be0$9bc5933e_at_monordinateur> Dear David, Melting while crossing the atmosphere is "superficial". Meteorites lose a major part of their weight (less for irons than stones) that burns away to ashes, but the inside of the meteorite remains at space temperature (i.e. abour -270°C). This is the main reason whay they often break into fragments in the atmosphere (because of high stresses due to temperature difference btween the inside and the "burning skin"), and actually this is what happened to Sikhote Alin, providing numerous fragments. As almost of all them show regmaglypts, this means that it happened in the high atmosphere, high enough to allow the fragments to keep on burning for a while. But the inside did not melt. For smaller fragments, the inside most probably heated up, but not to melting point. This is my understanding, and should I be wrong, please do not heasitate to let me know as I'm always open to learning more! Frederic Beroud www.meteoriteshow.com IMCA #2491 ----- Original Message ----- From: "David Hathaway" <dhathaway_at_peak.org> To: <meteorite-list_at_meteoritecentral.com> Sent: Tuesday, December 16, 2003 7:28 AM Subject: [meteorite-list] Patterns in Sikhote-Alin > I am a little curious about something..... > > I heard that the sikhote-alin meteorites have a Widmanstatten Pattern > although large and difficult to see. > > I have also heard that the regmaglypts are created when a molten piece cools > while airborne.. As nearly all the fragments I have seen have regmaglypts I > assume all these pieces have been molten. > > So after melting and recooling on Earth do they really maintain the pattern > or is it only present on pieces large enough not to melt? > > > > ______________________________________________ > Meteorite-list mailing list > Meteorite-list_at_meteoritecentral.com > http://www.pairlist.net/mailman/listinfo/meteorite-list > Received on Tue 16 Dec 2003 06:31:07 AM PST |
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