Mike,

Given the wide range of lithologies we are hearing about, all I am
saying it might be interesting to test the multiple lithologies and
confirm what you are saying. I am not suggesting anything about
multiple bodies or not, I don't have an opinion. I am simply
describing how you could provide geochem evidence to form a well
supported hypothesis. By the way, Laurence's BSE's on FB are
unequivocal L6 -- nice equilibrated chondrules!

Carl
*************************************
Carl B. Agee
Director and Curator, Institute of Meteoritics
Professor, Earth and Planetary Sciences
MSC03 2050
University of New Mexico
Albuquerque NM 87131-1126

Tel: (505) 750-7172
Fax: (505) 277-3577
Email: a...@unm.edu
http://meteorite.unm.edu/people/carl_agee/



On Thu, Jan 2, 2014 at 9:00 AM, Michael Farmer <m...@meteoriteguy.com> wrote:
> Carl, you you suggesting this might be from different fall? I was there less 
> than two weeks after the fall. I bought pieces as they were being found right 
> in front of us. When we showed up with cash the whole village ran around 
> picking up stones in 52 degree C (120f) heat. There were stones everywhere 
> including on the street. No one cared until we came with money. We found one 
> stone ourselves. Nearly every villager had stones. It is dead center India, 
> among the poorest places on earth. I saw 5 iron only pieces and numerous 
> partial iron and partial stone pieces.
> Whatever Katol is, (L6), it has large iron chunks inside and some become 
> complete individuals during the fall.
> I really would like I clarify that this piece is Katol, I was there as it was 
> found, we bought it seconds after the finder picked it up from beside his 
> house. Can we please accept that this is Katol, not another meteorite!
> Michael Farmer
>
> Sent from my iPhone
>
>> On Jan 2, 2014, at 8:48 AM, Carl Agee <a...@unm.edu> wrote:
>>
>> Hi MikeG and All:
>>
>> The iron might be from L6 if it turns out that the few silicates in it
>> (olivine and pyroxenes) have L6 geochem. You see that in the H-metal
>> from Yucca. Of course large metal masses are probably not as commonly
>> associated with L. Also if you had oxygen isotopes of the silicate
>> inclusions from the iron or for that matter oxygen isotopes of the
>> lithologies that seem to be more like achondrite, you could start to
>> sort out if it is all from the same meteoroid.
>>
>> Carl Agee
>> *************************************
>> Carl B. Agee
>> Director and Curator, Institute of Meteoritics
>> Professor, Earth and Planetary Sciences
>> MSC03 2050
>> University of New Mexico
>> Albuquerque NM 87131-1126
>>
>> Tel: (505) 750-7172
>> Fax: (505) 277-3577
>> Email: a...@unm.edu
>> http://meteorite.unm.edu/people/carl_agee/
>>
>>
>>
>> On Wed, Jan 1, 2014 at 7:06 PM, Galactic Stone & Ironworks
>> <meteoritem...@gmail.com> wrote:
>>> Hi Mike and List,
>>>
>>> Mike, and the behalf of countless others, I hope we hear that story
>>> one day.  I imagine it must have been pretty bad for you to say it was
>>> a "little scary".
>>>
>>> There are a predominance of stony lithologies, but Mike's iron is
>>> obviously not an L6 chondrite.  So what do we call a mass like Mike's
>>> superb iron shield?  Do we refer to his specimen as " Katol (L6)" or
>>> do we refer to it as something else?  Does Katol have some similarity
>>> with Almahata Sitta, in the sense that stones with different
>>> lithologies (and classifications) shared the same strewnfield?
>>>
>>> So, a majority of hand specimens show a curious lithology that is
>>> granular, shocked, and originating from the L-chondrite group.  Has
>>> anyone tried to plot the affinities from the specimens like Mike's
>>> that don't match the majority lithology?  I'd be curious if they also
>>> fit into the L-chondrite group, or, if they were xenoliths hitching a
>>> ride in the Katol rubble-pile.
>>>
>>> Good stuff.  It's about time that Katol gets some serious attention.  :)
>>>
>>> Best regards,
>>>
>>> MikeG
>>> --
>>> -------------------------------------------------------------
>>> Web - http://www.galactic-stone.com
>>> Facebook - http://www.facebook.com/galacticstone
>>> Twitter - http://twitter.com/galacticstone
>>> Pinterest - http://pinterest.com/galacticstone
>>> -------------------------------------------------------------
>>>
>>>
>>>
>>>
>>>
>>>> On 1/1/14, Michael Farmer <m...@meteoriteguy.com> wrote:
>>>> Yes, this piece is oriented heat shield shaped with countless flow lines 
>>>> and
>>>> bubbles on the thick backside crust. There are a couple of crystal-rich
>>>> sections. It is one of my favorite pieces in my collection, the adventure 
>>>> to
>>>> acquire was a little scary.
>>>> Laurence Garvie has taken many photos of it, I am sure he has incredible
>>>> photos I haven't seen. This photo was the only one I got.
>>>> The piece is still at ASU on loan, it will be on display at the Tucson
>>>> show.
>>>> Michael Farmer
>>>>
>>>> Sent from my iPhone
>>>>
>>>>> On Jan 1, 2014, at 5:27 PM, Carl Agee <a...@unm.edu> wrote:
>>>>>
>>>>> Oh, of course, this the metal-rich piece?
>>>>> *************************************
>>>>> Carl B. Agee
>>>>> Director and Curator, Institute of Meteoritics
>>>>> Professor, Earth and Planetary Sciences
>>>>> MSC03 2050
>>>>> University of New Mexico
>>>>> Albuquerque NM 87131-1126
>>>>>
>>>>> Tel: (505) 750-7172
>>>>> Fax: (505) 277-3577
>>>>> Email: a...@unm.edu
>>>>> http://meteorite.unm.edu/people/carl_agee/
>>>>>
>>>>>
>>>>>
>>>>>> On Wed, Jan 1, 2014 at 4:35 PM, Michael Farmer <m...@meteoriteguy.com>
>>>>>> wrote:
>>>>>> No chondrules.
>>>>>>
>>>>>> Sent from my iPhone
>>>>>>
>>>>>>> On Jan 1, 2014, at 4:25 PM, Graham Ensor <graham.en...@gmail.com>
>>>>>>> wrote:
>>>>>>>
>>>>>>> I think it is almost totally nickel iron and the marks are flow lines
>>>>>>> and small impact pits similar to those you find on Sikhote Alin...
>>>>>>>
>>>>>>> Graham
>>>>>>>
>>>>>>>> On Wed, Jan 1, 2014 at 8:30 PM, Carl Agee <a...@unm.edu> wrote:
>>>>>>>> Or perhaps the sphericals are vesiculation of fusion crust? I agree
>>>>>>>> with Jim, it would be nice to see some BSE images.
>>>>>>>>
>>>>>>>> Carl
>>>>>>>> *************************************
>>>>>>>> Carl B. Agee
>>>>>>>> Director and Curator, Institute of Meteoritics
>>>>>>>> Professor, Earth and Planetary Sciences
>>>>>>>> MSC03 2050
>>>>>>>> University of New Mexico
>>>>>>>> Albuquerque NM 87131-1126
>>>>>>>>
>>>>>>>> Tel: (505) 750-7172
>>>>>>>> Fax: (505) 277-3577
>>>>>>>> Email: a...@unm.edu
>>>>>>>> http://meteorite.unm.edu/people/carl_agee/
>>>>>>>>
>>>>>>>>
>>>>>>>>
>>>>>>>>> On Wed, Jan 1, 2014 at 1:28 PM, Carl Agee <a...@unm.edu> wrote:
>>>>>>>>> Beautiful oriented and flow lines! I assume all the circular and
>>>>>>>>> spherical shapes are chondrules peeking through the fusion crust?
>>>>>>>>>
>>>>>>>>> Thanks for sharing Mike!
>>>>>>>>>
>>>>>>>>> Carl
>>>>>>>>> *************************************
>>>>>>>>> Carl B. Agee
>>>>>>>>> Director and Curator, Institute of Meteoritics
>>>>>>>>> Professor, Earth and Planetary Sciences
>>>>>>>>> MSC03 2050
>>>>>>>>> University of New Mexico
>>>>>>>>> Albuquerque NM 87131-1126
>>>>>>>>>
>>>>>>>>> Tel: (505) 750-7172
>>>>>>>>> Fax: (505) 277-3577
>>>>>>>>> Email: a...@unm.edu
>>>>>>>>> http://meteorite.unm.edu/people/carl_agee/
>>>>>>>>>
>>>>>>>>>
>>>>>>>>>
>>>>>>>>> On Wed, Jan 1, 2014 at 11:44 AM, Jim Wooddell
>>>>>>>>> <jim.woodd...@suddenlink.net> wrote:
>>>>>>>>>> Thanks Jeff!
>>>>>>>>>>
>>>>>>>>>> Would love to see a polished window image as well as some BSE images
>>>>>>>>>> now!
>>>>>>>>>> Maybe Laurence or whoever has them can share!
>>>>>>>>>>
>>>>>>>>>> If this thing is going to have a paper published we may have to
>>>>>>>>>> wait!
>>>>>>>>>>
>>>>>>>>>>
>>>>>>>>>> Jim
>>>>>>>>>>
>>>>>>>>>>
>>>>>>>>>>
>>>>>>>>>>
>>>>>>>>>>
>>>>>>>>>>
>>>>>>>>>>> On 1/1/2014 11:35 AM, Jeff Grossman wrote:
>>>>>>>>>>>
>>>>>>>>>>> Mike's photo in posted in the database now.
>>>>>>>>>>>
>>>>>>>>>>> Jeff
>>>>>>>>>>>
>>>>>>>>>>> On 1/1/2014 1:19 PM, Jim Wooddell wrote:
>>>>>>>>>>
>>>>>>>>>>
>>>>>>>>>> --
>>>>>>>>>> Jim Wooddell
>>>>>>>>>> jim.woodd...@suddenlink.net
>>>>>>>>>> http://pages.suddenlink.net/chondrule/
>>>>>>>>>>
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