[meteorite-list] Two Questions
From: Gerald Flaherty <grf2_at_meteoritecentral.com>
Date: Tue May 24 18:42:18 2005 Message-ID: <004b01c560b1$cefa1160$2f01a8c0_at_Dell> Hi Walter, Eric and List, Would Martian Tectonic forces ie. subduction, be a possible mechanism to trap and transport atmospheric gases into the bowels of the planet, later to be be contained in a magma chamber? Just an odd thought. Jerry ----- Original Message ----- From: <star-bits_at_comcast.net> To: <meteorite-list_at_meteoritecentral.com> Sent: Tuesday, May 24, 2005 1:26 PM Subject: Re: [meteorite-list] Two Questions > Walter Branch wrote: > > <I been researching but I can't find the answers to two questions. > > First, what is the mechanism by which atmospheric gasses > are trapped in the formation of basalts? I have been doing some > lit reviews on martian meteorites and I find it interesting that some > were formed in magma chambers deep undergound. indeed, some are > thought to have formed several kilometers down. How does the > Martian atmosphere get trapped in cooling rock so far underground.> > > Hello Walter > > The mechanism for trapping gasses in Martian basalts is not entirely > clear. One method that has been proven is implanting during shock events, > such as being blasted off Mars. However there are some problems with this > as well such as sometimes the gasses are fractionated (Kr/Xe ratio changes > for instance). So although impact is likely part of the answer it isn't a > clear winner. Another suggestion is fluid (water) transplant, however the > gasses mostly reside in the water unaltered portions so this is likely not > the answer. Trapping of mantle gasses during cooling has been suggested, > but mantle reservoirs of gasses should have different ratios than > atmospheric. So the exact mechanism is undetermined. > > <Second, when determining Cosmic Ray Exposure ages, can atmospheric > fragmentation and ablation of a meteoroid affect the results from such > testing and if so, how are fragmentation and ablation taken into > consideration when determiniing CREs?> > > Yes fragmentation and ablation can affect the results and must be taken > into account. Cosmic rays generally penetrate 3-10 meters into asteroidal > bodies. Parts buried more than 10 meters or so receive almost no cosmic > ray exposure so their CRE age is zero. If depth isn't taken into account > a surface sample would show a older CRE than one at 5 meters. One method > of determining depth is with Neon isotopes which have been shown to have a > constant relationship with burial depth and cosmic ray exposure. So the > neon can be used to determine depth and the other elemental isotopes can > then be adusted for depth to give the CRE age. > > > -- > Eric Olson > ELKK Meteorites > http://www.star-bits.com > > >> Second try at posting this email: >> >> Hello Everyone, >> >> I been researching but I can't find the answers to two questions. >> >> First, what is the mechanism by which atmospheric gasses >> are trapped in the formation of basalts? I have been doing some >> lit reviews on martian meteorites and I find it interesting that some >> were formed in magma chambers deep undergound. indeed, some are >> thought to have formed several kilometers down. How does the >> Martian atmosphere get trapped in cooling rock so far underground. >> >> Second, when determining Cosmic Ray Exposure ages, can atmospheric >> fragmentation and ablation of a meteoroid affect the results from such >> testing and if so, how are fragmentation and ablation taken into >> consideration when determiniing CREs? >> >> Thanks to anyone who can help me understand these processes. >> >> -Walter Branch >> >> >> ______________________________________________ >> Meteorite-list mailing list >> Meteorite-list_at_meteoritecentral.com >> http://six.pairlist.net/mailman/listinfo/meteorite-list > ______________________________________________ > Meteorite-list mailing list > Meteorite-list_at_meteoritecentral.com > http://six.pairlist.net/mailman/listinfo/meteorite-list Received on Tue 24 May 2005 06:42:04 PM PDT |
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