Doug kindly wrote:

"Just a click away and an interested person without the materials and 
microscope can vicariously participate with Bernd's clear and colorful 
image of his nice thin section of Lodranite/Acapulcoite material."


Thank you, Doug. Much appreciated! Yes, that's one of my best pics
that I've taken so far in cross-polarized light and still without a gadget
to firmly attach the camera to the microscope, camera only hand-held!

Doug: "Bernd, could you kindly mention which of the grains were measured for 
those 
of us who want to confirm our little fun with a tape measure on our computer 
screens?"

I could but I won't ;-) Let me explain my rudeness: You have the field of view
in the upper right corner, so it's easy to figure out the rest - an easy 
exercise!

Doug quoting from C. Floss: "The simple bimodal classification of these 
meteorites
based primarily on petrographic criteria, which has been used to date, appears 
to be 
inadequate to describe this diverse group of samples, ..."

Hence I wrote and also quoted on Friday, Oct 26:
-----------------------------------------------------------------------------------------
But: It is not only grain size! ... and that's why this excerpt 
from an article in MAPS may be of interest in this context: 

TERRIBILINI D. et al. (2000) Evidence for common breakup events of the 
acapulcoites-lodranites and chondrites (MAPS 35-5, 2000, pp. 1043-1050). 

"GRA 95209 is considered a lodranite based on petrography (McCoy and 
Carlson, 1998), but Mittlefehldt and Lindstrom (1998) find that the bulk-rock 
composition is more similar to acapulcoites and quite different from that of 
lodranites. Thus, a clear-cut classification is difficult."

-----------------------------------------------------------------------------------------

Best wishes,

Bernd

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