Thanks for sharing your thoughts Elton. Especially about the thermal
expansion of some constituent(s).
All these working theories would be one heck of a multi-diciplinary:
chemistry, aerodynamic, thermodynamic, calculus, etc, problem beyond most
doctoral thesis work.
Yes, it would be. And
Hi all,
I was wondering, for those that are experienced with petrology, what
types of crystal twinning to do see the most in OC's?
Thanks!
Jim
--
Jim Wooddell
jim.woodd...@suddenlink.net
http://pages.suddenlink.net/chondrule/
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Visit the
The most common type of twinning in chondrules in unmetamorphosed chondrites
is found in low-Ca clinopyroxenes. It is polysynthetic twinning -- it looks
like the pyroxene grains have narrow stripes. These disappear when
temperatures go above 630 C or so and won't be found in orthopyroxene.
A geologic atlas of Africa, scale 1/5,000,000, that can be
either viewed online or downloaded as a high resolution
jpg can be found on the World Soil Information web site at
http://library.wur.nl/WebQuery/isric?q=%22Carte+G%C3%A9ologique+de+l%27Afrique%22
http://www.isric.eu/
Hi Friends and Collectors,
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Hello All,
Jim Wooddell inquired:
what types of crystal twinning do we see the most in OC's?
Alan Rubin kindly posted:
The most common type of twinning in chondrules in unmetamorphosed
chondrites is found in low-Ca clinopyroxenes. It is polysynthetic twinning
-- it looks like the pyroxene
Thanks Melinda, Alan and Bernd and all!
My next question would have been; Would it be safe to say if I see
polysynthetic twinning, odds are it's low-Ca cpx, but Melinda
pretty much answered this.
I have certainly seen this but the jury is out if I've seen other types
of twinning while playing
My pleasure, Jim!
Would it be safe to say if I see polysynthetic
twinning, odds are it's low-Ca cpx, ...
No, you might also be looking at multiple twinning of
plagioclase but in that case you may be pretty sure it
is *not* an unmetamorphosed chondrite!
Bernd
To: jim.woodd...@suddenlink.net
Okay. As I said and Andy said, we can find polysynthetic twins in low-Ca
clinopyroxene in type-2 and type-3 chondrites (those rocks that have not
been metamorphosed). We can actually find a few such twins surviving in
type-4 OC. We can see such twinning in plagioclase (also sometimes called
Dear List Members,
today I can present my new spectacular Sahara Iron.
NWA 6583 - Iron ungrouped with some rare silicate inclusions
(Enstatite and Diopside) in a polycrystalline iron textur.
Today's Meteorite Picture of the Day: HOW 88403
Contributed by: AMN
http://www.tucsonmeteorites.com/mpodmain.asp
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