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Improving Mindat.orgUnsubstantiated claims
21st Jan 2015 17:40 UTCReiner Mielke Expert
21st Jan 2015 17:59 UTCRob Woodside 🌟 Manager
21st Jan 2015 19:04 UTCAlfredo Petrov Manager
I did not approve the photo in question here, but when I am approving photos I generaly give the photographer the benefit of the doubt and assume their ID is correct, unless I see some specific reason to doubt it (wrong appearance, unlikely association, notoriously unreliable source...).
21st Jan 2015 19:22 UTCRob Woodside 🌟 Manager
From my limited experience I would raise Alfredo's 30% to more like 50% or higher and lower his 20% to 5% or less. Occasionally there are real howlers, like the wrong polymorph being identified by EDS, etc., but these are outliers and one of the reasons why 'whom and how' needs to be given in the captions or when adding a mineral to a locality.
Reiner, you do a lot of analysis. Do you think things are as bad as Alfredo suggests?
21st Jan 2015 19:49 UTCAlfredo Petrov Manager
We will always have to live with some uncertainty (which we strive to diminish). Those who insist on everything being absolutely black or white are going to have a great deal of frustration in mineralogy. There are so many young collectors who still live in a fantasy world of "This must be mineral X because it was analyzed!"
21st Jan 2015 20:17 UTCRalph S Bottrill 🌟 Manager
21st Jan 2015 21:20 UTCFrank Keutsch Expert
However, there are many cases, where analysis should be reliable.
I don't have any valid raguinite. All samples I got were just iron-sulfides in various stages of decay, including ones that looked exactly right!
The problem is knowing when this is the case.
Frank
21st Jan 2015 23:50 UTCRichard Gunter Expert
The RRUFF database has many examples of multi-phase crystals, especially among the sulphosalts. I like the one of the Mina El Cobre Tennantite-Tetrahedrite where multiple layers of varying chemistry have been deposited to make a euhedral crystal. In cases like that there is not even a name to call the crystal as it has so many distinct phases within it. Even XRD would not give an adequate answer to that texture, only elemental mapping would show the complexity.
22nd Jan 2015 00:14 UTCReiner Mielke Expert
22nd Jan 2015 03:27 UTCAlfredo Petrov Manager
22nd Jan 2015 10:37 UTCUwe Kolitsch Manager
For me, it's 40-60% and 20-40%, respectively. Haven't made any statistical evaluation, though.
22nd Jan 2015 16:18 UTCFrank Keutsch Expert
A typical case is sorbyite, which one can obtain samples of from Candelaria/Nevada, Sweden and other localities. Our work showed that none of the samples we got contained sorbyite as far as we could tell. For the Candelaria material what we found was a fine intergrowth of common minerals. With superficial EDS of unpolished samples the chemistry actually was fairly close to sorbyite! There are many similar cases.
Anyway, just thought I would chime in with this and support showing proof for vary rare minerals...
Frank
22nd Jan 2015 16:33 UTCReiner Mielke Expert
22nd Jan 2015 17:02 UTCRob Woodside 🌟 Manager
Gary Ansell used to buy specimens for the geological Survey of Canada and returning to Ottawa, Andy Roberts would x-ray them. At one species dealer's room Gary would go around checking labels and selecting specimens. When it came to settling up, the dealer, who knew Andy would check the pieces, started pulling them out of the flat saying, "I don't think you'll want this one. or this one, or..." About a third to a half of the selected specimens were removed. Even then Andy often couldn't find the supposed species.
22nd Jan 2015 17:41 UTCNorman King 🌟 Expert
22nd Jan 2015 18:30 UTCFrank Keutsch Expert
the specimens either stated Candelaria mine, or simply Candelaria. The problem is exactly as you state. Our work does not prove at all, that sorbyite does not exist there. However, it did not in our samples. I am fairly skeptical of any of the pictured sorbyites from there, but obviously I have no proof of this, and I am merely stating an opinion.
The issue I see is, who gets to decide whether a mineral is rare enough to require some form of proof. For sulfides and sulfosalts I have my own experience but it is clearly not objective due to the limited dataset.
Here is the list of rare minerals I could not find in my last analytical run:
- shandite
- argentotennantite
- tischendorffite
- sederholmite
- nowackiite
- nisbite
- garavellite
- berthierite (not really rare but it was zinkenite)
- koutekite
- argentotennantite (other locality)
- moschellandsbergite
- stromeyerite
- laffitite
The ones that were correct:
- samsonite
- germanocolusite
- clausthalite
- villamaninite
- hauchecornite
- anilite (probably)
- guanajuatite
- arsenohauchecornite (who was that one from I wonder!!)
- krennerite
- galkhaite
Anyway, just some observations...
Frank
22nd Jan 2015 20:13 UTCHenri Koskinen Expert
Henri
.
24th Jan 2015 04:21 UTCRock Currier Expert
24th Jan 2015 04:54 UTCMatthew Stanley
-------------------------------------------------------
"It may encourage people to get analysis done on their samples thereby improving the quality of the database."
I'm really liking this thread, but this sentence caught my eye. I am not a scientist. I am not a dealer. I don't collect "high end" specimens because I can't afford them. Where can an average Joe go to get a mineral analyzed, and how much would it cost? Seems to me like it would only be worth it for really expensive specimens.
Was this statement meant to exclude us average Joes from contributing to the database? If not, that's fine, but that's how it came across. If I'm wrong and an analysis is only a few bucks, then I'll gladly start analyzing my collection.
24th Jan 2015 05:06 UTCRock Currier Expert
24th Jan 2015 14:31 UTCReiner Mielke Expert
A basic EDS analysis is $10 US and is available to anyone here: http://kaygeedeeminerals.com/sem-eds_service If you want a more thorough and detailed analysis I would recommend this for $40:http://www.attminerals.com/mineral_identification.htm : This desire for analysis only applies to rare species which most collectors are not likely to encounter or be interested in (because they are not usually very attractive).
24th Jan 2015 15:48 UTCChester S. Lemanski, Jr.
24th Jan 2015 16:38 UTCFrank Craig
I have been following and have taken an interest in this thread. Most common minerals do not "need" analysis beyond their physical properties as the necessary proof. There are exceptions to this, such as the amphiboles and perhaps the pyroxenes - physical properties alone will not always help with the mineral species. Chemistry (and atomic structure) is essential to the amphibole classification, for example. I want to point out that EDS (alone) cannot always provide the necessary accuracy for such "proof". You have to be careful when choosing a person/lab to do the work, especially if you are not familiar with the technique. There are differences in the way detectors are designed as well as each manufacturers software used in displaying and interpreting the spectra (this applies to the operator as well).
Having said that, both Reiner and I know that EDS can be an indispensible aid in the identification of a mineral. So, I guess the major point here is to be very selectful of which minerals you want to have analysed as well as the person/lab doing the work. Otherwise you could end up spending excessive amounts of money for someone to tell you something that you already knew, or for data that is misleading.
I hope this is some help.
Regards
Frank
24th Jan 2015 17:08 UTCMatthew Stanley
Thank you for the replies. It is far cheaper than I was expecting. I will have to do some further research on this and perhaps take advantage in the future. Thank you for such an educational thread!
24th Jan 2015 17:50 UTCFrank Craig
24th Jan 2015 19:31 UTCAlfredo Petrov Manager
It's more expensive ($40) but a bit more reliably quantitative. He also does PXRD (powder X-ray diffraction) for the same price (for which you need to provide a sample about half the size of a grain of rice), and results usually come within 48 hours. He can also check the presence of various elements by wet chemistry and by arc spectroscope.
It should also be noted that many collectors get specimens analyzed free of charge by mineralogists at universities or museums. The disadvantage of that is that mineralogists at public institutions tend to be very overworked and often will sit on your specimen for months before doing the analysis, or may never do it at all unless it happens to be from a locality or a mineral group that they are particularly interested in. If you want fast results, it's better to use one of the commercial services.
24th Jan 2015 20:51 UTCTony Nikischer 🌟 Manager
I must agree with others that EDS is an excellent tool to aid in identification, and it used in my lab on a regular basis. However, complex minerals may often require two or more analytical techniques to unequivocally identify the phase. The skills of the operator (both mineralogical as well as technical) are important, as is the suitability of the type equipment being used for the specific mineral. Two articles appeared in Min Rec years ago (one on XRD and one by yours truly re: EDS and WDS) that are still useful today. The emergence of Raman and other techniques, along with the construction of accurate databases, are game-changers today.
26th Jan 2015 18:02 UTCRob Woodside 🌟 Manager
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Privacy Policy - Terms & Conditions - Contact Us / DMCA issues - Report a bug/vulnerability Current server date and time: April 24, 2024 00:42:26