[meteorite-list] Ordinary chondrites - decimal metamorphic grade question
From: Darryl Pitt <darryl_at_meteoritecentral.com>
Date: Thu, 17 Dec 2009 08:19:33 -0500 Message-ID: <B3291016-794B-4A66-82D4-A9C50D5A58BD_at_dof3.com> Good Morning, Thank you so much for this! Finally get the nuances... Darryl On Dec 17, 2009, at 5:50 AM, Jeff Grossman wrote: > Types 2 and 3 are describing two different parameters. Type 2 (and > 1) means that a meteorite has experienced aqueous alteration. > Because such effects are prominent in the CI, CM and CR groups, > nearly all of them are traditionally (since the 1960s) described as > types 1 and 2. Types 3-6 are traditionally used to describe > metamorphic effects in chondrite groups where thermal processing has > been important, such as CO, CV, CK, OCs, ECs, etc. Although most > meteorites in the first list above are hydrated but unmetamorphosed > and most meteorites in the second list are metamorphosed but > unhydrated, there is crossover that leaves us without an adequate > vocabulary to describe. Some CM and related chondrites have been > heated to levels similar to a type 3.2 chondrite, yet they are still > called type 2 due to alteration. Some low-type-3 ordinary and CV > chondrites have hydrated phases and Ni-bearing sulfides like a type > 2 chondrite might, yet they are called type 3.0 to distinguish them > from more-heated group members. > > So, when I say that most CR chondrites are type 3.00, I mean that > their thermal histories are similar to those of type 3.00 ordinary > or CO chondrites; they have never gotten very hot for very long. > But most CR chondrites are ALSO type 2. Most CM chondrites are type > 2 (alteration) AND type 3.00 (metamorphism). But somehow, alteration > trumps metamorphism for carbonaceous chondrites and nobody calls > them type 3.00 even thought this describes them well. Strangely, > when a CR chondrite lacks alteration, many people are happy to call > it type 3 (e.g., MET 00426). But when an ordinary chondrite is > hydrated, nobody would ever think of calling it type 2 (e.g., > Semarkona). > > This is called a lousy nomenclature system. > > jeff g. > > At 05:25 AM 12/17/2009, Jeff Kuyken wrote: >> Hi Jeff, >> >> Inrteresting stuff indeed. One thing just caught my attention >> though. You mentioned that "CR chondrites which are mostly type >> 3.00" which I have not heard of before. The Met Bull lists nearly >> all as CR2, some as just CR and an odd CR1. My crude understanding >> of type-2 vs type-3 is that type-2 never received thermal >> alteration whereas type-3 is where that starts. Am I wrong there? >> >> So would CR3.00 tell us that the particular meteorite in question >> did not go through any thermal metamorphism? How would that vary >> from CR2? >> >> Thanks, >> >> Jeff >> >> >> ----- Original Message ----- From: "Jeff Grossman" <jgrossman at usgs.gov >> > >> To: <Meteorite-list at meteoritecentral.com> >> Sent: Thursday, December 17, 2009 3:12 AM >> Subject: Re: [meteorite-list] Ordinary chondrites - decimal >> metamorphic grade question >> >> >> The hundredths place is only defined for type 3s >> that are lower than type 3.2. This is because >> there is a lot of variation in metamorphic >> effects in the low end of the range, too much to >> cram into just types 3.0 and 3.1. Initially, I >> define 4 new classes: 3.00, 3.05, 3.10 and 3.15 >> (Grossman and Brearley 2005, in >> MAPS). Subsequently Kimura, I and others have >> realized that there are subtle variations that >> may require more categories between 3.00 and >> 3.05, e.g. Semarkona as a type 3.01, as compared >> with CR chondrites which are mostly type 3.00. >> >> You do not need specialized equipment other than >> an electron microprobe to determine >> this. However, with high-resolution FE-SEM >> imaging, you can see structures in the metal and >> olivine that also give this classification >> information. Raman spectroscopy also helps classify meteorites in >> this range. >> >> Jeff >> >> At 11:04 AM 12/16/2009, Matt Morgan wrote: >>> Since Darryl brought up his incredible LL3.05, I have to ask how >>> does/can one classify the metamorphic grade to the to the tenths >>> or now the hundredths of a decimal? I have had some tell me this >>> is subjective and others say you need specialized equipment. >>> Please, any researchers, explain. >>> >>> Darryl- >>> I don't mean to pick on your material, but it is a question that >>> has been nagging me for sometime and you stirred my brain! >>> >>> Thanks in advance! >>> Matt >>> ---------------------- >>> Matt Morgan >>> Mile High Meteorites >>> http://www.mhmeteorites.com >>> P.O. Box 151293 >>> Lakewood, CO 80215 USA >>> >>> -----Original Message----- >>> From: Darryl Pitt <darryl at dof3.com> >>> Date: Wed, 16 Dec 2009 10:35:38 >>> To: Jeff Grossman<jgrossman at usgs.gov> >>> Cc: <Meteorite-list at meteoritecentral.com> >>> Subject: Re: [meteorite-list] Ordinary chondrites - rarest to the >>> most >>> common classes >>> >>> >>> >>> Get ready for NWA 5717..... >>> >>> Initially "anomalous," the classification had to be changed to >>> "ungrouped" as it was too difficult to determine what it was >>> anomalous >>> to. 3.05 subtype. More to follow.... >>> >>> >>> >>> >>> >>> On Dec 16, 2009, at 10:26 AM, Jeff Grossman wrote: >>> >>> > At 09:27 AM 12/16/2009, Chladnis Heirs wrote: >>> >> Indeed, >>> >> >>> >> it's for the first time, that I read that R-chondrites are >>> included >>> >> in the >>> >> OC-group. If so, why exactly them and not the K-chondrites, the >>> >> Carbonaceous >>> >> from grade 3-6, the ungrouped and the enstatite chondrites too? >>> > >>> > I didn't say they ARE included in the OCs... I said that I thought >>> > they should be. As far as I know, I am alone in this opinion. >>> There >>> > are only two Kakangari-like chondrites, and I am not prepared to >>> put >>> > them anywhere. I'm not sure what the rest of the question means, >>> > but many ungrouped chondrites can be and are associated with a >>> major >>> > class, as in "ungrouped carbonaceous chondrite". >>> > >>> > jeff >>> > >>> > >>> >> >>> >> >valuable type of OC from a >>> >> >scientific perspective is petrologic type 3.00-3.01 >>> >> >>> >> Where one has to say, that it's maybe too early to say that, >>> >> Because the classification with decimal places, (even with two!), >>> >> is a >>> >> relatively new occurrence - most classifiers seems still to >>> prefer >>> >> to use a >>> >> simple "3" - so that in case, there are still a lot known >>> type-3ers >>> >> awaiting >>> >> to be revisited regarding the degree of their (un)equilibration. >>> >> >>> >> But I agree - "Ordinary" is a somewhat misleading term, >>> >> - as the ordinary chondrites have told us most about the origin >>> and >>> >> formation of the solar system, the planets and ourselves, more >>> than >>> >> any iron >>> >> or any lunar rock! >>> >> >>> >> Keep that always in mind, if you are tempted, now in the end of >>> the >>> >> desert-era and the decreed end of meteorite finding in so many >>> >> countries, >>> >> with all their weird and fancy exotic types, to wrinkle your nose >>> >> about the >>> >> "ugly" ordinary 25$-a-kilo-chunk from NWA-wonderland! >>> >> Rare as brilliants they are - and they were our beginnings! >>> >> >>> >> Happy holidays to all! >>> >> Martin >>> >> >>> >> >>> >> -----Urspr?ngliche Nachricht----- >>> >> Von: meteorite-list-bounces at meteoritecentral.com >>> >> [mailto:meteorite-list-bounces at meteoritecentral.com] Im Auftrag >>> von >>> >> Jeff >>> >> Grossman >>> >> Gesendet: Mittwoch, 16. Dezember 2009 11:33 >>> >> An: Meteorite-list >>> >> Betreff: Re: [meteorite-list] Ordinary chondrites - rarest to the >>> >> most >>> >> common classes >>> >> >>> >> I agree with Doug... the rarest and most valuable type of OC >>> from a >>> >> scientific perspective is petrologic type 3.00-3.01, from any >>> of the >>> >> chemical groups. Only one is known... Semarkona. If we take a >>> more >>> >> expansive definition of "ordinary chondrite" than most of my >>> rather >>> >> conservative colleagues are normally willing to accept, I would >>> say >>> >> that >>> >> the rarest group of OCs is the R chondrites (only ~100 are >>> known and >>> >> many of those are paired). In addition, a number of unique >>> ungrouped >>> >> meteorites are OC-like. But again, I don't know of any >>> colleagues >>> >> who >>> >> agree with me that R chondrites are in the OC class. [I would say >>> >> that >>> >> the OC class has two clans, the H-L-LL clan and the R clan]. >>> >> >>> >> Jeff >>> >> >>> >> Mexicodoug wrote: >>> >> > Hi Melanie and thanks for the enthusiasm you add to the >>> list ... >>> >> > >>> >> > Here's a high to low sorting of the "ordinary chondrites", >>> for over >>> >> > 32,000 meteorites: >>> >> > >>> >> > 22.0% L6 ("most common") >>> >> > 19.9% H5 >>> >> > 12.9% L5 >>> >> > 12.3% H4 >>> >> > 11.5% H6 >>> >> > 7.8% LL5 >>> >> > 4.2% LL6 >>> >> > 3.3% L4 >>> >> > 2.2% H3 >>> >> > 2.0% L3 >>> >> > 0.8% LL4 >>> >> > 0.8% LL3 >>> >> > 0.1% L7 >>> >> > 0.1% LL7 >>> >> > 0.03% H7 ("least common") >>> >> > >>> >> > But this "common" and "rare" is a misleading label. That is a >>> >> harder >>> >> > question if you look too closely at the deails and consider >>> >> > inhomogeneous and brecciated ordinary chondrites. That can all >>> >> become >>> >> > somewhat unique if you ask the right person. Then there are the >>> >> motley >>> >> > crew of ungrouped ordinary chondrites where it is hard to >>> >> generalize. >>> >> > Some may be a weak classification while others might truly be >>> weird >>> >> > ("rare"). >>> >> > >>> >> > Just a few notes: the H7, L7, LL7 types are not widely used >>> in the >>> >> > literature and border on impact melts, so I'd take them with a >>> >> grain >>> >> > of salt unless someone goes postal on me in which case they are >>> >> right >>> >> > in whatever they say. The way I listed these, the meteorites >>> are >>> >> > counted by the lowest number and won't show up in the higher >>> >> thermal >>> >> > (metamorphosed) levels. In other words, for example, an >>> LL3.8-6 is >>> >> > counted with the LL3's. >>> >> > >>> >> > If you have a special meteorite, it can sometimes be a "rarer" >>> >> type if >>> >> > you start to split hairs, like H3.8 instead of just grouping it >>> >> within >>> >> > the H3's, but there is some degree of arbitrariness to this. >>> The >>> >> > tendency is that more virgin Solar system stuff (closer and >>> closer >>> >> > 3.00) is more special and like a holy grail ("rare" in a >>> sense) to >>> >> > some who study that - since it is more representative of the >>> >> original >>> >> > material before water and heat were added and did their >>> thing. From >>> >> > hat we can try to get the proof we need to work out early >>> formation >>> >> > processes and theorize on the related dynamics happening. By >>> this >>> >> > logic, and considering it is a very studied meteorite, the >>> precious >>> >> > meteorite SEMARKONA (LL3.00 or is it 3.01 :-)), a witnessed >>> fall >>> >> from >>> >> > India, is rather unique being the only one with that 3.00 >>> >> > classification, which makes it super intact since formation and >>> >> > especially interesting to experts, and most notably Dr. Jeff >>> >> Grossman >>> >> > who reviewed and updated its classification upon careful study. >>> >> > >>> >> > By another measure, the "common" ordinary chondrite, L5, >>> Canadian >>> >> > witnessed fall, VILNA, is one of those very few special >>> meteorites >>> >> > that was imaged during atmospheric entry and a precise orbit >>> was >>> >> > determined. It was not too far from Buzzard Coulee, and what >>> >> makes it >>> >> > even more special is that it was classified from a (although >>> >> witnesses >>> >> > heard pieces whizzing around) 94 milligram fragment with fusion >>> >> crust. >>> >> > The only other specimen found was a 48 milligram piece! This >>> >> becomes a >>> >> > wild anecdote of a meteorite tale when one considers that the >>> >> bolide >>> >> > passed directly over the only camera recording the sky for 500 >>> >> miles >>> >> > (over 800 km) and headed for the newly constructed and >>> world's only >>> >> > UFO landing site which had been built for the Canadian >>> Centennial >>> >> > exposition in St. Paul, Alberta, where it showered sparks >>> >> > ("retro-rockets" to some folks). In case you wondered, I >>> believe >>> >> the >>> >> > Japanese classified on Antarctic meteorite with 10 >>> milligrams, if >>> >> you >>> >> > can believe that! >>> >> > >>> >> > So what actually makes a meteorite rare can turn into a >>> matter of >>> >> > semantics and who you ask. Even the scale of 3 to 6 (or 7) is >>> >> somewhat >>> >> > arbitrary and just looks for convenient thermally changed >>> cairns >>> >> along >>> >> > the path toward melting. So if we went the other way, if H, L, >>> >> and LL >>> >> > correspond to only three parent bodies, the frequency of the >>> types >>> >> > follows: >>> >> > >>> >> > H 45.0% >>> >> > L 40.6% >>> >> > LL 14.3% >>> >> > >>> >> > Hope this helps a little with that general question! >>> >> > >>> >> > Kind wishes, >>> >> > Doug >>> >> > >>> >> > >>> >> > >>> >> > >>> >> > >>> >> > >>> >> > >>> >> > >>> >> > >>> >> > >>> >> > >>> >> > >>> >> > >>> >> > >>> >> > >>> >> > -----Original Message----- >>> >> > From: Melanie Matthews <miss_meteorite at yahoo.ca> >>> >> > To: meteorite-list at meteoritecentral.com >>> >> > Sent: Tue, Dec 15, 2009 7:01 am >>> >> > Subject: [meteorite-list] Ordinary chondrites - rarest to the >>> most >>> >> > common classes >>> >> > >>> >> > >>> >> > G'mornin' listites,, >>> >> > What is the least common type of ordinary chondrite, as well >>> as the >>> >> > most common? >>> >> > >>> >> > >>> >> > >>> >> > Thanks >>> >> > ----------- >>> >> > Melanie >>> >> > IMCA: 2975 >>> >> > eBay: metmel2775 >>> >> > Known on SkyRock Cafe as SpaceCollector09 >>> >> > >>> >> > Unclassified meteorites are like a box of chocolates... you >>> never >>> >> know >>> >> > what >>> >> > you're gonna get! >>> >> > >>> >> > >>> >> > >>> >> >>> >__________________________________________________________________ >>> >> > Looking for the perfect gift? Give the gift of Flickr! >>> >> > >>> >> > http://www.flickr.com/gift/ >>> >> > >>> >> >______________________________________________ >>> >> > http://www.meteoritecentral.com >>> >> > Meteorite-list mailing list >>> >> > Meteorite-list at meteoritecentral.com >>> >> > http://six.pairlist.net/mailman/listinfo/meteorite-list >>> >> > >>> >> >______________________________________________ >>> >> > http://www.meteoritecentral.com >>> >> > Meteorite-list mailing list >>> >> > Meteorite-list at meteoritecentral.com >>> >> > http://six.pairlist.net/mailman/listinfo/meteorite-list >>> >> > >>> >> >>> >> >>> >> -- >>> >> Dr. Jeffrey N. Grossman phone: (703) 648-6184 >>> >> US Geological Survey fax: (703) 648-6383 >>> >> 954 National Center >>> >> Reston, VA 20192, USA >>> >> >>> >> >>> >>______________________________________________ >>> >> http://www.meteoritecentral.com >>> >> Meteorite-list mailing list >>> >> Meteorite-list at meteoritecentral.com >>> >> http://six.pairlist.net/mailman/listinfo/meteorite-list >>> >> >>> >>______________________________________________ >>> >> http://www.meteoritecentral.com >>> >> Meteorite-list mailing list >>> >> Meteorite-list at meteoritecentral.com >>> >> http://six.pairlist.net/mailman/listinfo/meteorite-list >>> > >>> > Dr. Jeffrey N. Grossman phone: (703) 648-6184 >>> > US Geological Survey fax: (703) 648-6383 >>> > 954 National Center >>> > Reston, VA 20192, USA >>> > >>> > >>> >______________________________________________ >>> > http://www.meteoritecentral.com >>> > Meteorite-list mailing list >>> > Meteorite-list at meteoritecentral.com >>> > http://six.pairlist.net/mailman/listinfo/meteorite-list >>> >>> ______________________________________________ >>> http://www.meteoritecentral.com >>> Meteorite-list mailing list >>> Meteorite-list at meteoritecentral.com >>> http://six.pairlist.net/mailman/listinfo/meteorite-list >> >> Dr. Jeffrey N. Grossman phone: (703) 648-6184 >> US Geological Survey fax: (703) 648-6383 >> 954 National Center >> Reston, VA 20192, USA >> >> >> ______________________________________________ >> http://www.meteoritecentral.com >> Meteorite-list mailing list >> Meteorite-list at meteoritecentral.com >> http://six.pairlist.net/mailman/listinfo/meteorite-list >> > > Dr. Jeffrey N. Grossman phone: (703) 648-6184 > US Geological Survey fax: (703) 648-6383 > 954 National Center > Reston, VA 20192, USA > > > ______________________________________________ > http://www.meteoritecentral.com > Meteorite-list mailing list > Meteorite-list at meteoritecentral.com > http://six.pairlist.net/mailman/listinfo/meteorite-list Received on Thu 17 Dec 2009 08:19:33 AM PST |
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