Good Question: "What about Olivine, would the melt point of Olivine be higher 
than the glass?"

Molten olivine at "silica glass" melting(aka"fusion")temperatures.

Not at all as olivine has the highest fusion temperature in Bowen's Reaction 
Series(BRS). Thus it is the first to crystalize and precipitate out of magma.  
This is why it is used as a refactory material in making fire bricks. Olivine 
fuses at 1890*C, well above where iron fuses.  The two minerals making up 
olivine: forsterite and fayalite are very close in fusion temperatures as to be 
negligible in general discussion.

Silica, aka "quartz" has the lowest fusion temperature in BRS(1600*C +) and 
thusly rare in meteorites. That fact and this:When olivine is forced to react 
with quartz in any of several situations such as reheating,deep mantle 
pressures,extended cooling cycles,etc., the two minerals reform to produce 
enstatite. (Does the H and E chondrite composition and their parent bodies make 
more sense?)

When this quality of olivine and it's implications sink in, one might 
experience the "Eureka" effect.  It goes very, very far in explaining why 
meteorite petrology is the way it is:Especially, pallasites.

Elton

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