Hello All,
Gao, Chergach, Pultusk, and other ordinary chondrites often have their
impact melt portions ignored when being characterized.  Chelyabinsk
would be the most recent obvious example of this -- "LL5 S4 W0"
Except, when you read the petrographic description:

"...A significant portion (1/3) of the stones consist of a dark,
fine-grained impact melt containing mineral and chondrule fragments.
Feldspar is well developed and practically isotropic. No high-pressure
phases were found in the impact melt. There are black-colored thin
shock veins in both light and dark lithologies."

http://www.lpi.usra.edu/meteor/metbull.php?code=57165

We collectors see impact melt and think it's cool, but it's secondary
information for the classification, I think.

Regards,
Jason

www.fallsandfinds.com


On Wed, Oct 30, 2013 at 6:35 AM, Jim Wooddell
<jim.woodd...@suddenlink.net> wrote:
> On 10/30/2013 6:02 AM, Marc Fries wrote:
>>
>> Let  me try that again with a more accurate Subject line...
>> Hi Marc!
>
> Looking at the pictures and the lack of information in the bulletin, this
> one would be worthy of another stab at classification!  Happy (b) and (c)
> could use some new work too!
>
>
>
> Jim
>
>
>
>
>> On Oct 29, 2013, at 11:27 AM, Marc Fries wrote:
>>
>>> Howdy all
>>>
>>>      I'm looking for a meteorite to buy or borrow for a scientific study.
>>> Does anyone have a piece of Happy(a)?  It is listed as an H3 but appears to
>>> be an impact melt, at least in part.  Please contact me off-list at
>>> mfri...@hotmail.com
>>>
>>> Cheers,
>>> Marc Fries
>>>
>
>
> --
> Jim Wooddell
> jim.woodd...@suddenlink.net
> http://pages.suddenlink.net/chondrule/
>
>
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