Zero valent dominant member of Pyrochlore Group (original) (raw)
A variety of Pyrochlore Group
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Photos of Zero valent dominant member of Pyrochlore Group (10)
Zero valent dominant member of Pyrochlore Group GallerySearch Photos of Zero valent dominant member of Pyrochlore Group
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Samiresy, Tritriva, Betafo District, Vakinankaratra, Madagascar
Samiresite, etc.
Samiresy, Tritriva, Betafo District, Vakinankaratra, Madagascar
Samiresy, Tritriva, Betafo District, Vakinankaratra, Madagascar
Samiresy, Tritriva, Betafo District, Vakinankaratra, Madagascar
Samiresite, etc.
Samiresy, Tritriva, Betafo District, Vakinankaratra, Madagascar
Samiresy, Tritriva, Betafo District, Vakinankaratra, Madagascar
Samiresy, Tritriva, Betafo District, Vakinankaratra, Madagascar
Samiresite, etc.
Samiresy, Tritriva, Betafo District, Vakinankaratra, Madagascar
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About Zero valent dominant member of Pyrochlore GroupHide
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Formula:
A2Nb2(O,OH)6Z
First Recorded Locality:
ⓘ Panda Hill, Mbeya, Mbeya Region, Tanzania
A variety of Pyrochlore Group
A pyrochlore group member where there is a cation deficit comprised mainly of H2O or site vacancies. This name is used to describe any pyrochlore where it is not possible to specify more accurately than this.
Unique IdentifiersHide
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Mindat ID:
40348 (as Zero valent dominant member of Pyrochlore Group)
3316 (as Pyrochlore Group)
Long-form identifier:
mindat:1:1:40348:9 (as Zero valent dominant member of Pyrochlore Group)
mindat:1:1:3316:5 (as Pyrochlore Group)
GUID
(UUID V4):
306e3813-990f-4f71-8e66-9283d0c02885 (as Zero valent dominant member of Pyrochlore Group)
3a54fe93-40ce-4d2b-baa3-52597b88699b (as Pyrochlore Group)
Chemistry of Zero valent dominant member of Pyrochlore GroupHide
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Mindat Formula:
A2Nb2(O,OH)6Z
Elements listed:
H, Nb, O - search for minerals with similar chemistry
First Recorded Occurrence of Zero valent dominant member of Pyrochlore GroupHide
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ⓘ Panda Hill, Mbeya, Mbeya Region, Tanzania
Synonyms of Zero valent dominant member of Pyrochlore GroupHide
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Bariopyrochlore (of Hogarth 1977)
Yttrobetafite (of Hogarth 1977) (in part)
Varieties of Zero valent dominant member of Pyrochlore GroupHide
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Samiresite | A Pb-bearing variety of Zero valent dominant member of Pyrochlore GroupDescribed and named by Lacroix (1912) as a betafite with a content of Pb. It was found in a metamict state. Named after the locality, the Samiresy pegmatite in the Betafo district, V... |
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Common AssociatesHide
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Associated Minerals Based on Photo Data:
6 photos of Zero valent dominant member of Pyrochlore Group associated with Titan-uranoan Oxycalciopyrochlore | (Ca,U,Na)2(Nb,Ti,Ta)2O6(O,OH) |
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Other InformationHide
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Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.
Internet Links for Zero valent dominant member of Pyrochlore GroupHide
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mindat.org URL:
https://www.mindat.org/min-40348.html
Please feel free to link to this page.
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References for Zero valent dominant member of Pyrochlore GroupHide
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Reference List:
Christy, A. G., Atencio, D. (2013) Clarification of status of species in the pyrochlore supergroup. Mineralogical Magazine, 77 (1) 13-20 doi:10.1180/minmag.2013.077.1.02
Localities for Zero valent dominant member of Pyrochlore GroupHide
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This map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the symbol to view information about a locality. The symbol next to localities in the list can be used to jump to that position on the map.
Locality ListHide
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- This locality has map coordinates listed. - This locality has estimated coordinates. ⓘ - Click for references and further information on this occurrence. ? - Indicates mineral may be doubtful at this locality. - Good crystals or important locality for species. - World class for species or very significant. (TL) - Type Locality for a valid mineral species. (FRL) - First Recorded Locality for everything else (eg varieties). Struck out - Mineral was erroneously reported from this locality. Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).
All localities listed without proper references should be considered as questionable.