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- Q3905061 subject Q7318171.
- Q3905061 subject Q7478371.
- Q3905061 subject Q8946220.
- Q3905061 abstract "Pimelite was discredited as a mineral species by the International Mineralogical Association (IMA) in 2006, in an article which suggests that “pimelite” specimens are probably willemseite (which is approved), or kerolite (which is also discredited). This was a mass discreditation, and not based on any re-examination of the type material (assuming any exists). Nevertheless, a considerable number of papers have been written, verifying that pimelite is a nickel-dominant smectite. It is always possible to redefine a mineral wrongly discredited.The mineral was erroneously assumed to be a nickel-rich talc in a paper published in the American Mineralogist in 1979, but it had already been determined to be a smectite as early as 1938, and this was confirmed in another article in the American Mineralogist in 1966. Both nickel-bearing talc and nickel dominant smectite occur at the type locality, Szklary, Ząbkowice Śląskie County, Lower Silesia, Poland.".
- Q3905061 thumbnail Pimelite_2.jpg?width=300.
- Q3905061 wikiPageWikiLink Q102151.
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- Q3905061 wikiPageWikiLink Q7318171.
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- Q3905061 wikiPageWikiLink Q7478371.
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- Q3905061 wikiPageWikiLink Q8946220.
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- Q3905061 name "Pimelite".
- Q3905061 type ChemicalSubstance.
- Q3905061 type Mineral.
- Q3905061 type ChemicalObject.
- Q3905061 type Thing.
- Q3905061 type Q7946.
- Q3905061 comment "Pimelite was discredited as a mineral species by the International Mineralogical Association (IMA) in 2006, in an article which suggests that “pimelite” specimens are probably willemseite (which is approved), or kerolite (which is also discredited). This was a mass discreditation, and not based on any re-examination of the type material (assuming any exists). Nevertheless, a considerable number of papers have been written, verifying that pimelite is a nickel-dominant smectite.".
- Q3905061 label "Pimelite".
- Q3905061 depiction Pimelite_2.jpg.
- Q3905061 name "Pimelite".