In a message dated 20-May-02 1:54:37 PM Pacific Daylight Time, 
[EMAIL PROTECTED] writes:

<Since the planets are formed from chondritic asteroids, I don't think you can
 rule them out just because the meteorite is a chondrite.> 

So are you proposing that there is remnant chondritic material on earth from 
its formation 4.5 billion years ago?  Although the specifics maybe different 
Mercury and Venus formed through the same differentiation/core formation 
process as earth.  The probability of remnant chondritic material on Mercury 
and  Venus is about the same as it is for earth.
 
<Since the olivine crystals are only found in an iron matrix, that should 
 be your first big hint. >

Could be, except that olivine is found as massive formations of large olivine 
crystals without an iron matrix, just not in meteorites.   One notable 
location 
is the San Carlos Apache reservation where unaltered mantle material 
was erupted to the surface.  It is now mined for gem quality olivine, 
commonly 
known as peridot.   So the question remains if there are olivine crystals 60 
to 
100 kilometers deep on earth (the depth of the peridot source) why haven't 
we found meteorites composed of just olivine crystals?  There is no currently 
accepted answer.

Somewhere I have some of this mantle material from Kilbourne hole in southern 
New Mexico.   If I can find it I will post a picture tomorrow.

Eric Olson
http://www.star-bits.com

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