[meteorite-list] Geophysics, meteorites, and Electron microscopy-QUESTION

2011-09-09 Thread Shawn Alan
Carl and Anne and Listers.

Carl thank you for your explanation on SEM analysis. As for testing meteorites 
I assume they have to be a thin slice from what I had read. Now are there other 
tests where you can take 30mg of the meteorite and get the same result? But I 
would assume this would be destructive process because the fragment might have 
to be crushed up into power form. If this is the case, what equipment would be 
involved or process and is it more feasible to have the specimen in a thin 
section form.

Why I ask is that some meteorites are super rare, and in order to have a SEM 
test, one must have a thin slice and from my understanding that takes about a 
gram or so of the meteorite in order for that to happen. Not good for the 
meteorite nor for the collection it comes from if its rare.

As for the electron microscopy I asked Santa for one and also a scientist. I 
hope I have been good enough this year to get one in my stocking.

Shawn Alan 
IMCA 1633 
eBaystore 
http://shop.ebay.com/photophlow/m.html 






[meteorite-list] Geophysics, meteorites, and Electron microscopy-QUESTIONCarl 
Agee agee at unm.edu 
Thu Sep 8 09:36:36 EDT 2011 


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microscopy-QUESTION 
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Hi Shawn, 

It's actually the electron microprobe that gives the quantitative 
analyses needed for classification of stony meteorites. The data is 
usually output in tables of oxide component concentrations in weight 
percent, totalling hopefully, to approximately 100%. The microprobe 
software lets you select which elements (expressed as oxides) to 
analyze and assign the element to one of the probe's spectrometers. 
The software will also give atomic concentrations to check for mineral 
stoichiometry. For metals and sulfides the output is usually in 
element percent. Calibration of the probe against known standards 
(minerals or compounds similar to what are in your meteorite) precedes 
the microprobe session and can take several hours. Once the probe is 
calibrated, you are good to go on your first unknown meteorite that 
would normally be in a polished thin section or polished epoxy-cast 
probe mount. Because the calibration is time consuming it is 
economical to do several samples in a single session. Sessions can go 
on for hours, and you can even set up a collection of x-y coordinates 
and let the auto-feature of the probe analyze different spots all 
night long. In the morning a stack of data would be be waiting for 
your perusal and evaluation. 

Of course there are other tests and analyses that contribute to a high 
quality meteorite classification, which include visual textural 
information from both polarizing microscope and SEM observation (e.g. 
shock effects, percent mineral make-up, weathering), and of course 
macroscopic characteristics seen in the hand sample. Oxygen isotopes 
are also great to have, especially as a "court of appeals" for 
borderline cases or for anomalous meteorites that don't fall into 
clear-cut geochemical groups. There are many other techniques such as 
isotopic age dating, cosmic ray exposure, bulk trace element analyses, 
and so on that enhance the characterization of a stony meteorite, but 
the electron microprobe is the work horse for most classification 
data. 

Someone who has done work on Ensisheim (LL6) and Saint-Séverin (LL6) 
could give a better answer that I can about the their subtle 
differences and whether the microprobe can distinguish between them, 
but my guess would be yes, especially when combined with SEM imaging. 

The length of time for classification from start to finish, including 
the write-up is variable. The initial ID or categorization of an 
unknown doesn't have to take long, that's what emerges in the first 
hour or so of microprobe analysis. But often, for a water-tight, 
authoritative classification, a second probe session may be required. 
Plus a lot of the time is spent puuzzling through the data and 
narrowing down the possibilities. It's like detective work, and 
personally I find it immensely engaging. 

Hope this helps, 

Carl Agee 


-- 
Carl B. Agee 
Director and Curator, Institute of Meteoritics 
Professor, Earth and Planetary Sciences 
MSC03 2050 
University of New Mexico 
Albuquerque NM 87131-1126 

Tel: (505) 750-7172 
Fax: (505) 277-3577 
Email: agee at unm.edu 
http://epswww.unm.edu/iom/pers/agee.html 

-
 
On Wed, Sep 7, 2011 at 4:47 PM, Shawn Alan  wrote: 

> Hello Carl and Listers 

> 

> Great post on scanning electron microscope (SEM) process, now does this 
> process also ID the whole classification of the meteorite which is used for 
> classifying 

Re: [meteorite-list] Geophysics, meteorites, and Electron microscopy-QUESTION

2011-09-09 Thread Carl Agee
Shawn,

A probe mount can be much less than a gram but it depends on the
texture of the sample. For example, I just finished some preliminary
work on a new unclassified shergottite and had separated out a ~0.4
gram fragment for various tests, and used only about a third of that
for the probe mount because it has a uniform grain size and is pretty
homogeneous. If I am working on a polymict breccia, like a howardite,
larger and multiple fragments may be needed. The ideal case is if you
buy a polished thin section to go along with your hand sample, that
way you don't have to mess with your display piece. The probe
mounts/thin sections can also be used for ion probe work or laser
ablation ICPMS which are both great for trace elements, and of course
SEM for great images.

Tell Santa he can pick up a new Cameca or JEOL electron probe for
under $1M. The scientists are cheaper -- haha!

Carl Agee

-- 
Carl B. Agee
Director and Curator, Institute of Meteoritics
Professor, Earth and Planetary Sciences
MSC03 2050
University of New Mexico
Albuquerque NM 87131-1126

Tel: (505) 750-7172
Fax: (505) 277-3577
Email: a...@unm.edu
http://epswww.unm.edu/iom/pers/agee.html


On Thu, Sep 8, 2011 at 4:54 PM, Shawn Alan  wrote:
> Carl and Anne and Listers.
>
> Carl thank you for your explanation on SEM analysis. As for testing 
> meteorites I assume they have to be a thin slice from what I had read. Now 
> are there other tests where you can take 30mg of the meteorite and get the 
> same result? But I would assume this would be destructive process because the 
> fragment might have to be crushed up into power form. If this is the case, 
> what equipment would be involved or process and is it more feasible to have 
> the specimen in a thin section form.
>
> Why I ask is that some meteorites are super rare, and in order to have a SEM 
> test, one must have a thin slice and from my understanding that takes about a 
> gram or so of the meteorite in order for that to happen. Not good for the 
> meteorite nor for the collection it comes from if its rare.
>
> As for the electron microscopy I asked Santa for one and also a scientist. I 
> hope I have been good enough this year to get one in my stocking.
>
> Shawn Alan
> IMCA 1633
> eBaystore
> http://shop.ebay.com/photophlow/m.html
>
>
>
>
>
>
> [meteorite-list] Geophysics, meteorites, and Electron microscopy-QUESTIONCarl 
> Agee agee at unm.edu
> Thu Sep 8 09:36:36 EDT 2011
>
>
> Previous message: [meteorite-list] Geophysics, meteorites, and Electron 
> microscopy-QUESTION
> Next message: [meteorite-list] Ad and new website announcement
> Messages sorted by: [ date ] [ thread ] [ subject ] [ author ]
>
> Hi Shawn,
>
> It's actually the electron microprobe that gives the quantitative
> analyses needed for classification of stony meteorites. The data is
> usually output in tables of oxide component concentrations in weight
> percent, totalling hopefully, to approximately 100%. The microprobe
> software lets you select which elements (expressed as oxides) to
> analyze and assign the element to one of the probe's spectrometers.
> The software will also give atomic concentrations to check for mineral
> stoichiometry. For metals and sulfides the output is usually in
> element percent. Calibration of the probe against known standards
> (minerals or compounds similar to what are in your meteorite) precedes
> the microprobe session and can take several hours. Once the probe is
> calibrated, you are good to go on your first unknown meteorite that
> would normally be in a polished thin section or polished epoxy-cast
> probe mount. Because the calibration is time consuming it is
> economical to do several samples in a single session. Sessions can go
> on for hours, and you can even set up a collection of x-y coordinates
> and let the auto-feature of the probe analyze different spots all
> night long. In the morning a stack of data would be be waiting for
> your perusal and evaluation.
>
> Of course there are other tests and analyses that contribute to a high
> quality meteorite classification, which include visual textural
> information from both polarizing microscope and SEM observation (e.g.
> shock effects, percent mineral make-up, weathering), and of course
> macroscopic characteristics seen in the hand sample. Oxygen isotopes
> are also great to have, especially as a "court of appeals" for
> borderline cases or for anomalous meteorites that don't fall into
> clear-cut geochemical groups. There are many other techniques such as
> isotopic age dating, cosmic ray exposure, bulk trace element analyses,
> and so on that enhance the charact

Re: [meteorite-list] Geophysics, meteorites, and Electron microscopy-QUESTION

2011-09-08 Thread Doug Ross
Thanks for the free tutorial, Dr. Agee!  That was really enlightening.  :)

Doug Ross




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Re: [meteorite-list] Geophysics, meteorites, and Electron microscopy-QUESTION

2011-09-08 Thread Carl Agee
Hi Shawn,

It's actually the electron microprobe that gives the quantitative
analyses needed for classification of stony meteorites. The data is
usually output in tables of oxide component concentrations in weight
percent, totalling hopefully, to approximately 100%. The microprobe
software lets you select which elements (expressed as oxides) to
analyze and assign the element to one of the probe's spectrometers.
The software will also give atomic concentrations to check for mineral
stoichiometry. For metals and sulfides the output is usually in
element percent. Calibration of the probe against known standards
(minerals or compounds similar to what are in your meteorite) precedes
the microprobe session and can take several hours. Once the probe is
calibrated, you are good to go on your first unknown meteorite that
would normally be in a polished thin section or polished epoxy-cast
probe mount. Because the calibration is time consuming it is
economical to do several samples in a single session. Sessions can go
on for hours, and you can even set up a collection of x-y coordinates
and let the auto-feature of the probe analyze different spots all
night long. In the morning a stack of data would be be waiting for
your perusal and evaluation.

Of course there are other tests and analyses that contribute to a high
quality meteorite classification, which include visual textural
information from both polarizing microscope and SEM observation (e.g.
shock effects, percent mineral make-up, weathering), and of course
macroscopic characteristics seen in the hand sample. Oxygen isotopes
are also great to have, especially as a "court of appeals" for
borderline cases or for anomalous meteorites that don't fall into
clear-cut geochemical groups. There are many other techniques such as
isotopic age dating, cosmic ray exposure, bulk trace element analyses,
and so on that enhance the characterization of a stony meteorite, but
the electron microprobe is the work horse for most classification
data.

Someone who has done work on Ensisheim (LL6) and Saint-Séverin (LL6)
could give a better answer that I can about the their subtle
differences and whether the microprobe can distinguish between them,
but my guess would be yes, especially when combined with SEM imaging.

The length of time for classification from start to finish, including
the write-up is variable. The initial ID or categorization of an
unknown doesn't have to take long, that's what emerges in the first
hour or so of microprobe analysis. But often, for a water-tight,
authoritative classification, a second probe session may be required.
Plus a lot of the time is spent puuzzling through the data and
narrowing down the possibilities. It's like detective work, and
personally I find it immensely engaging.

Hope this helps,

Carl Agee


--
Carl B. Agee
Director and Curator, Institute of Meteoritics
Professor, Earth and Planetary Sciences
MSC03 2050
University of New Mexico
Albuquerque NM 87131-1126

Tel: (505) 750-7172
Fax: (505) 277-3577
Email: a...@unm.edu
http://epswww.unm.edu/iom/pers/agee.html

-
On Wed, Sep 7, 2011 at 4:47 PM, Shawn Alan  wrote:
> Hello Carl and Listers
>
> Great post on scanning electron microscope (SEM) process, now does this 
> process also ID the whole classification of the meteorite which is used for 
> classifying meteorite for the Meteoritcal Bulletin database? I know alot of 
> school are discontinuing classifying meteorites is UNM also doing the same?
>
> Question if someone wanted this service to be done on a meteorite, how much 
> would it cost, cause these days money talks and helps everyone out when it 
> comes to classifying meteorites or confirming that the meteorite is the 
> meteorite suggested to be. Also can this process determine the difference 
> between Ensisheim (LL6) and Saint-Séverin (LL6) by the cosmic ray exposure or 
> terrestrial age. These two meteorites look identical and some can fake it. 
> Does SEM also cover that test or is that a different test? Lastly how long 
> does it take for you to classify a new meteorite from start to finish if its 
> a stony meteorite?
>
>
> Shawn Alan
> IMCA 1633
> eBaystore
> http://shop.ebay.com/photophlow/m.html
>
>
>
>
> [meteorite-list] Geophysics, meteorites, and Electron microscopyCarl Agee 
> agee at unm.edu
> Tue Sep 6 12:27:18 EDT 2011
>
>
> Previous message: [meteorite-list] Geophysics, meteorites, and Electron 
> microscopy
> Next message: [meteorite-list] FW: High Noon!
> Messages sorted by: [ date ] [ thread ] [ subject ] [ author ]
>
> A scanning electron microscope (SEM) is great for high magnification
> images that also contain information about the chemical composition 

[meteorite-list] Geophysics, meteorites, and Electron microscopy-QUESTION

2011-09-07 Thread Shawn Alan
Hello Carl and Listers

Great post on scanning electron microscope (SEM) process, now does this process 
also ID the whole classification of the meteorite which is used for classifying 
meteorite for the Meteoritcal Bulletin database? I know alot of school are 
discontinuing classifying meteorites is UNM also doing the same? 

Question if someone wanted this service to be done on a meteorite, how much 
would it cost, cause these days money talks and helps everyone out when it 
comes to classifying meteorites or confirming that the meteorite is the 
meteorite suggested to be. Also can this process determine the difference 
between Ensisheim (LL6) and Saint-Séverin (LL6) by the cosmic ray exposure or 
terrestrial age. These two meteorites look identical and some can fake it. Does 
SEM also cover that test or is that a different test? Lastly how long does it 
take for you to classify a new meteorite from start to finish if its a stony 
meteorite?


Shawn Alan 
IMCA 1633 
eBaystore 
http://shop.ebay.com/photophlow/m.html 




[meteorite-list] Geophysics, meteorites, and Electron microscopyCarl Agee agee 
at unm.edu 
Tue Sep 6 12:27:18 EDT 2011 


Previous message: [meteorite-list] Geophysics, meteorites, and Electron 
microscopy 
Next message: [meteorite-list] FW: High Noon! 
Messages sorted by: [ date ] [ thread ] [ subject ] [ author ] 

A scanning electron microscope (SEM) is great for high magnification 
images that also contain information about the chemical composition of 
the different minerals in meteorites. SEM is also a quick way to do a 
qualitative analysis of a sample, say for example, detecting nickel in 
iron meteorites with energy dispersive spectroscopy (EDS). 

My instrument of choice for definitive ID of stony meteorites is the 
electron microprobe. This also has SEM imaging capability. In less the 
hour, on a calibrated electron microprobe, I can make a definitive ID, 
although unequilbrated chondrites can take more time to narrow down 
the possibilities. Some of the key geochemical quantities that help in 
categorizing are, Fe/Mn of olivines and pyroxenes, the fayalite and 
ferrosilite content of the olivines and pyroxenes, the 
anorthite-albite content of plagioclse, and a few other parameters, 
plus the percent mineralogy and other textural characteristics. 

So for a simple example lunar olivines usually have higher Fe/Mn than 
terrestrial basalt olivines. Check out this page's second figure for 
an overview of Fe/Mn versus plagioclase content of planetary basalts: 
http://www.imca.cc/mars/martian-meteorites.htm 

Carl Agee 

-- 
Carl B. Agee 
Director and Curator, Institute of Meteoritics 
Professor, Earth and Planetary Sciences 
MSC03 2050 
University of New Mexico 
Albuquerque NM 87131-1126 

Tel: (505) 750-7172 
Fax: (505) 277-3577 
Email: agee at unm.edu 
http://epswww.unm.edu/iom/pers/agee.html 

l-- 
Geophysics, meteorites, and Electron microscopy 

Barb and Jake Baker bakers5acres at frontiernet.net 
Tue Sep 6 10:50:46 EDT 2011 

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Could someone tell me, in Microscopy 101 language: How is an electron 
microscope used in the study of meteorites? Using electron microscopy - 
what differences are apparent between meteorites and terrestrial rocks? For 
instance what are the microscopy differences between lunar basalt and 
terrestrial basalt? 

Thanks 





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[meteorite-list] Geophysics, meteorites, and Electron microscopy

2011-09-06 Thread Carl Agee
A scanning electron microscope (SEM) is great for high magnification
images that also contain information about the chemical composition of
the different minerals in meteorites. SEM is also a quick way to do a
qualitative analysis of a sample, say for example, detecting nickel in
iron meteorites with energy dispersive spectroscopy (EDS).

My instrument of choice for definitive ID of stony meteorites is the
electron microprobe. This also has SEM imaging capability. In less the
hour, on a calibrated electron microprobe, I can make a definitive ID,
although unequilbrated chondrites can take more time to narrow down
the possibilities. Some of the key geochemical quantities that help in
categorizing are, Fe/Mn of olivines and pyroxenes, the fayalite and
ferrosilite content of the olivines and pyroxenes, the
anorthite-albite content of plagioclse, and a few other parameters,
plus the percent mineralogy and other textural characteristics.

So for a simple example lunar olivines usually have higher Fe/Mn than
terrestrial basalt olivines. Check out this page's second figure for
an overview of Fe/Mn versus plagioclase content of planetary basalts:
http://www.imca.cc/mars/martian-meteorites.htm

Carl Agee

--
Carl B. Agee
Director and Curator, Institute of Meteoritics
Professor, Earth and Planetary Sciences
MSC03 2050
University of New Mexico
Albuquerque NM 87131-1126

Tel: (505) 750-7172
Fax: (505) 277-3577
Email: a...@unm.edu
http://epswww.unm.edu/iom/pers/agee.html

l--
Geophysics, meteorites, and Electron microscopy

Barb and Jake Baker bakers5acres at frontiernet.net
Tue Sep 6 10:50:46 EDT 2011

Previous message: [meteorite-list] [AD] Canyon Diablo 2,7 kg. CHEAP!
Messages sorted by: [ date ] [ thread ] [ subject ] [ author ]


Could someone tell me, in Microscopy 101 language: How is an electron
microscope used in the study of meteorites? Using electron microscopy -
what differences are apparent between meteorites and terrestrial rocks? For
instance what are the microscopy differences between lunar basalt and
terrestrial basalt?

Thanks
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[meteorite-list] Geophysics, meteorites, and Electron microscopy

2011-09-06 Thread Barb and Jake Baker
Could someone tell me, in Microscopy 101 language:  How is an electron 
microscope used in the study of meteorites?  Using electron microscopy - 
what differences are apparent between meteorites and terrestrial rocks? For 
instance what are the microscopy differences between lunar basalt and 
terrestrial basalt?


Thanks

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