You are too kind, Carl.  Let me address your questions inside your quote:

--- On Fri, 6/5/09, [email protected] <[email protected]> wrote:
Q: I have a few follow-up questions for you; If an Earth meteorite (terrene) 
were to return back to Earth, would we be able to identify it correctly?

A: Yes and No.  IF you look at the locations of recent major impacts(80 Million 
years or later) and consider the bedrock/ target rock-type at the launch 
origin. It narrows the filed of possible rock types.

The best candidate is Reis crater in Germany which lies on limestone.  The 
Canadian shield cluster and Popogui impacts are far too (old we think) and that 
leaves Chesapeake, Chicxulub, The un-named crater in the North Sea off Scotland 
and Wetumpka Al.  So far as I know all these excavated down to deep crystalline 
basement rock so most have a component of igneous rock mixed with the 
sedimentary kinds.  

Statistically the older the impact the more likely that any orbitally ejected 
material will have already fallen back long before mankind existed. Someone 
somewhere did a study of the physics on what sized crater had enough energy to 
eject material at escape velocity and seems like it was in the range of 5 
miles/8km someone with a better database might chime in.

Chicxulub target rocks included slates,sandstone, sulfate rocks and weathered 
lavas .  The sulfates are generally too fragile. Sandstone has a wide range of 
hardness and is more difficult to predict launch integrity and space survival. 
Quartzite remains the best candidate for launch, survival and recognition but 
Popagui in Siberia is over 200 myo(?)(Geoff Notkin knows, he fed the mosquitoes 
there one summer). The crystalline bedrocks are usually pyroxene, mica, 
feldspar, and silica(quartz) mixtures.  Earth rocks tend to have larger grain 
and clast sizes.  Certain grain sizes could only come from Earth as no other 
planet other than Venus could grow them.

That leaves a granitoid rocks and quartzite for best chance of survival and 
recognition.  A fusion crust on those: granite --white to brown with specs of 
black.  Quartzite probably a frosty clear glass coating.

When Limestone is heated it does not melt but turns into highly soluble lime 
(CaO) and Carbon dioxide ( CO2)...so there isn't a fusion crust.  It would be 
white until the first rain.

Q: That is to say would we not simply ASSume it came from the moon? As a
> moon meteorite would also have Earth air or isotopes?

A: Owing that the Earth and Moon came from the same stock we share the same 
isotope abundances so there is no isotope ratio test to differentiate them. 
Again grain size and clast sizes would be larger on material from Earth

We make new supposed Lunar meteorite discoveries with new
> materials all the time. So again I ask is there a way to be
> certain where it came from? I ask because if is not mostly
> plagioclase, it seems to me most investigators would simply
> toss it aside and say; it is not a meteorite, that is a rind
> or weathered Earth rock not fusion crust.

Yes there is so much industrial slag about even regular moon meteorites look 
like it but I will keep looking for out of place rocks.  Moon material from the 
Mares is hard to differentiate from earth basalt save for the clasts.  The 
feldspars could come from anywhere in New Hampshire, Vermont-- actually most 
all of New England, so again anyone looking would need a very trained eye.  I 
think the first identified Earthite will be the one that crashes through a roof 
and makes someone take a hard look.

Right now unless it were very very old due to an extremely large orbit that 
took 700-1300 million years to decay-- there are no candidate craters on Earth 
that are in feldspar-rich bedrock that come to mind. 

Actually Nininger(?) or someone--found a limestone object that was reported to 
be a fall and in fact he thought it to be a meteorite but it was so unlike 
anything known it was unable to prove it.  The where-a-bouts of the object is 
unknown. It is listed as a psuedo-meteorite in the Natural History (British) 
Museum's Catalog of meteorites

Q: So, another
> question would be this; if it clearly has a fusion crust
> complete with the gas bubbles would there be a way to prove
> it is in fact a genuine fusion crust???

The short answer: Cosmic ray tracks and enriched tritium from solar wind would 
be proof that the material had been in space. Fusion crust in my book is over 
rated as "proof" owing to the wide occurrence of industrial glass so widely 
spread on Earth AND poorly understood/recognized accurately as everyone claims 
fusion crust when in fact the crust is long gone and they are looking at the 
ablation surface. An ablation surface can look like water or wind-worn surfaces.

You are Welcome, Elton
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