Hi Bernd and Greg,

It is so strange that is for sure. I don't know what it is but it has
about the same metal as an H chondrite and the olivine of a diogenite
but the (possible) chondrule of a lodranite. Go figure....

Whatever it is I have never seen anything quite like it.




On Mon, Oct 5, 2009 at 3:32 PM,  <[email protected]> wrote:
> Ruben wrote: Ureilite maybe?
>
> Hi Ruben and List,
>
> Yes, maybe a ureilite like the Hupés' NWA 2624 but where are the triple 
> junctions?
> You would expect a lot of olivine grains with "sets" of three olivine grains 
> that meet
> in triple junctions of 120° (3 x 120° = 360°).
>
> Bernd
>
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