AW: [meteorite-list] Tafassasset classification
From: Norbert Classen <trifid_at_meteoritecentral.com>
Date: Thu Apr 22 10:06:55 2004 Message-ID: <NCBBKMGDKLMGIBALJOFCMENBCOAA.trifid_at_timewarp.de> Hi Frank, John, and List, While discussing Tafassasset, Dr. Otto explained to me in much detail the fundamental difference between chondrites and achondrites - something that is quite obvious in viewing various thin sections. First, achondrites - including primitive achondrites - exhibit much larger crystals than any chondrite due to igneous melting and recrystalization processes. The matrix of a type 6 or type 7 chondrite is very fine grained compaired to primitive achondrites. True chondritic matter has never been melted by igneous processes, and it looks vastly different from achondritic matter through the microscope. Tafassasset is a very good example - it shows a coarse-grained crytalline matrix that exhibitis all features of a total igneous recrystalization of it's chondritic precursor - one of these features are the triple-junctions of the olivine, usually found in brachinites. Dr. Otto showed me various thin sections of chondrites, including CR's, and there is nothing even remotely resembling this coarse grained, recrystalized texture. However, it is very similar to Divnoe, Zag (b), and the brachinites. To put it short: the crystal size and texture of a primitive achondrite are very different from type 7 chondrites - even I could see this without much guideance. However, the elemental compositions and REE patterns of primitive achondritic matter remain more or less chondritic - and hence these meteorites have been defined as primitive achondrites. But since they have been completely recrystalized it's impossible to say that they have been an CR, CO, or CV etc. before recrystallization. You can't take some similarities, such as the O-isotopic composition and the approximate amount of metal, to justify such a wild guess. With the same logic you could guess that the aubrites might be lunar or terrestrial meteorites. Now, what to make of the "relict chondrules" in Tafassasset - and what about relict chondrules in general? Dr. Otto explained to me that relict chondrules have escaped the process of recrystalization and remained more or less intact in a few primitive achondrites, such as NWA 725 (Tissemoumine), and Monument Draw, both acapulcoites. The structures in Tafassasset, however, look much more like something Dr. Otto calls "Sammelkristalle" - I don't find the proper translation, sorry - something like agglomerates of crystals that usually form during melting and recrystalization processes; Dr. Otto even showed me similar agglomerates in thin sections of terrestrial igneous rocks. Well, does that mean that these structures can't be interpreted as relict chondrules? Yes and no. Dr. Otto said that he has seen these structures, too, but there's one fundamental fact that makes him doubt that they could be relict chondrules. Most of these structures are primarily composed of plagioclase poikilitically enclosing minor olivines and pyroxenes, often accompanied by nickel-iron metal. The predominance of plagioclase in these agglomerates is strange since chondrules usually aren't composed of plagioclase. There would be just one possibility - glas-rich or glas chondrules that have been transformed into plagioclase during the melt process. But, according to Dr. Otto, this is rather improbable and nothing more than a wild guess. It's much more probable that these structures are indeed "Sammel- kristalle", and no relict chondrules. Anyway, even if it should be relict chondrules in the end, Tafassasset should be regarded per definition as a quite typical primitive achondrite because of its completely recrystalized, coarse-grained texture. Now, I hope this helps to explain Dr. Otto's point of view, and the difference between type 7 chondrites and primitive achondrites. To me, all of this sounded more than convincing. I just hope that I've been able to present his view coherently in my poor English. And sorry for this lengthy email... Best regards, Norbert > -----Original Message----- > Von: meteorite-list-admin_at_meteoritecentral.com > [mailto:meteorite-list-admin_at_meteoritecentral.com]Im Auftrag von fcressy > Gesendet: Donnerstag, 3. Oktober 2002 06:08 > An: meteorite-list_at_meteoritecentral.com; John Divelbiss > Betreff: Re: [meteorite-list] Tafassasset classification > > > Hi John and all, > > I believe that, in general, primative achondrites are no longer chondrites > in that the rock has rxperienced melting and chondrules are no longer > present. The rock has recrystallized and it has a crystalline texture. > However, compositionally they remain the same as the parent chondrite > material. So texturally they are achondrites, compositionally they are > chondrites. If I remember correctly from my acapulcoite samples, a lot of > metal is present between the crystals. In a regular differented > achondrite, > the metal has separated out as has other material and the resultant > composition of the rock is significanrtly different from the parent body. > As for the difference between a petrographic grade 7 and a primative > achondrite, I agree that this line is fuzzy. Grade 7 chondrites > should still > have relict chondrules present. However, I believe that at least one > acapulcoite (NWA725) also contains relict chondrules. > This is my understanding of the subject. Hope it helps a bit but feel free > to correct me if I'm not understanding this correctly. > Regards, > Frank > > ----- Original Message ----- > From: John Divelbiss <j.divelbiss_at_worldnet.att.net> > > > Frank, > > > > I understand the description of the primitive achondrite...including the > > types you mention. > > > > From that statement in Nortons book, they are still chondrites...just > > overdone a bit. What line did they cross to be called > achondrites? And how > > does it relate to Tafassasset being also called a CR7? > > > > John > > > > ----- Original Message ----- > > From: "fcressy" <fcressy_at_prodigy.net> > > To: "John Divelbiss" <j.divelbiss_at_worldnet.att.net>; "Norbert Classen" > > <trifid_at_timewarp.de>; "Bernd Pauli HD" > > <bernd.pauli_at_lehrer.uni-karlsruhe.de>; "Svend Buhl" <svendbuhl@web.de> > > Cc: <meteorite-list_at_meteoritecentral.com> > > Sent: Wednesday, October 02, 2002 10:55 PM > > Subject: Re: [meteorite-list] Tafassasset classification > > > > > > > Hello John and all, > > > Regarding your primative achondrite question, Norton's > "Encyclopedia of > > > Meteorites" has a page dedicated to the subject (P. 165). He > states that > > > "primative achondrites have achondrite textures but still retain > something > > > of their chondritic composition." and that they "are transitional > between" > > > chondrites and achondrites. As examples of primative achondrites, he > uses > > > acapulcoites, lodranites and winonaites. > > > Hope this helps. > > > Frank > > > > > > > > > > > > > > > ----- Original Message ----- > > > From: John Divelbiss <j.divelbiss_at_worldnet.att.net> > > > To: Norbert Classen <trifid_at_timewarp.de>; Bernd Pauli HD > > > <bernd.pauli_at_lehrer.uni-karlsruhe.de>; Svend Buhl <svendbuhl@web.de> > > > Cc: <meteorite-list_at_meteoritecentral.com> > > > Sent: Wednesday, October 02, 2002 5:05 PM > > > Subject: Re: [meteorite-list] Tafassasset classification > > > > > > > > > > Hello All, > > > > > > > > Primitive is primitive! Help me to understand the differences > > > please. > > > > > > > > Is the argument about where the line(s) should be drawn between a > > > chondrite > > > > (that is "really" differentiated...like a 7) versus a primitive > > achondrite > > > > (that is not quite differentiated enough to be called a achondrite)? > > > > > > > > Is there really a 7 category and why? > > > > > > > > Are primitive achondrites now considered differentiated enough to be > > > > distinguished from a highly changed chondrite? small versus coarse > > grains > > > in > > > > matrix? > > > > > > > > How is this line drawn? mineral makeup, level of glass, age, grain > > > > size/changes, etc. ? > > > > > > > > Lots of questions with this story. > > > > > > > > Alain would have something to say about all this. Ann > Black, is there > a > > > > position written from his corner? > > > > > > > > > > > > John > > > > > > > > > ______________________________________________ > Meteorite-list mailing list > Meteorite-list_at_meteoritecentral.com > http://www.pairlist.net/mailman/listinfo/meteorite-list > Received on Thu 03 Oct 2002 08:06:12 AM PDT |
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