[meteorite-list] Two Questions
From: MarkF <mafer_at_meteoritecentral.com>
Date: Tue May 24 19:15:55 2005 Message-ID: <003301c560b6$89f7f410$b940fc04_at_MAF> Hi Eric and List Its my understanding that an atmosphere is created as much by volcanism as anything else (gravity attracting the gases along with the denser matter which makes up a globe, ect). Via volcanoes, gases like H2 O ,SO2 ,CO2 are all generated during volcanism and found in atmospheres, so finding them in mantle rock isn't such a hard thing to consider. Mark Ferguson ----- Original Message ----- From: <star-bits_at_comcast.net> To: "Gerald Flaherty" <grf2_at_verizon.net>; <meteorite-list_at_meteoritecentral.com> Sent: Tuesday, May 24, 2005 6:54 PM Subject: Re: [meteorite-list] Two Questions > No, there is no evidence of plate techtonics on Mars and therefor no > subduction. > > -- > Eric Olson > ELKK Meteorites > http://www.star-bits.com > > >> 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 >> >> ______________________________________________ >> 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 07:15:54 PM PDT |
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