[meteorite-list] Question on new NWA 2828 paleometeorite

stan . laser_maniac at hotmail.com
Wed Sep 6 22:05:30 EDT 2006


while i have no offical word yet it seems as though the nwa 2828 is the same 
material as the 'second lithology' from the E6/7 i bought in tucson (nwa 
2965). I recived the material from two seperate dealers and submitted 
speicmins of both lithologies to NAU. at first it was asusmed that both the 
light colored and dark veined material was the same fall - primarily because 
they were aparently recovered from the same site and the diffrence in 
lithology was the result of widly differing weathering between the two sorts 
of material. Since then I have been contacted by NAU and informed that the 
'second lithology' material is infact a totally diffrent enstatite 
meterotie.

now this is where things get strange. there is material that exists that 
CLEARLY and i mean CLEARLY shows BOTH the light blue occasional chondrule 
lithology, AND the dark brown highly veined lithology int he same piece. 
Despite the vastly differring apearances of the stones, it is because of 
these examples that I thought the finding of the material all being the same 
was logical.

so that means there are one or two possibilities now:

there are two totally seperate large enstatite falls recovered in overlaping 
strewnfields with SOME of one fall weathered in a way to partially resemble 
the other

OR (my current pet theory not supported by any of the science guys) is that 
this is all from one big meteorite that is an E3-7

so no offical word either way - but thats my two cents for what it's worth.


>
>Hi all,
>I can't help but wonder when I look at the new paleo EL3 offering by Greg
>Hupe (likely the same as Stan's fresh EL7 slices and Marcin Cimala's 
>yet-to-
>be classified MC024) how anyone suspected it as a meteorite in the first
>place. It was underground, stuck to rhyolite cobbles, shows no crust or 
>fresh
>metal. How was it identified? There must be an interesting story in its
>discovery. Anyone?
>Thanks,
>Bob
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