Vanadio-laumontite
A variety of Laumontite
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Formula:
CaAl2Si4O12 · 4H2O
A V-bearing variety of laumontite.
It was descrided as a yellow-red substance deposited on first-generation calcite and covered with very tiny second-generation calcite crystals; it also constitutes a cement of the green Cu-V minerals (Antipov, 1908).
Seemingly needs a modern reinvestigation.
Originally reported from Tyuya-Muyun Cu-V-U Deposit (Radium Mine), Fergana Valley, Osh Oblast, Kyrgyzstan.
It was descrided as a yellow-red substance deposited on first-generation calcite and covered with very tiny second-generation calcite crystals; it also constitutes a cement of the green Cu-V minerals (Antipov, 1908).
Seemingly needs a modern reinvestigation.
Originally reported from Tyuya-Muyun Cu-V-U Deposit (Radium Mine), Fergana Valley, Osh Oblast, Kyrgyzstan.
Unique Identifiers
Mindat ID:
4140 (as Vanadio-laumontite)
2340 (as Laumontite)
2340 (as Laumontite)
Long-form identifier:
mindat:1:1:4140:5 (as Vanadio-laumontite)
mindat:1:1:2340:1 (as Laumontite)
mindat:1:1:2340:1 (as Laumontite)
Chemistry of Vanadio-laumontite
Mindat Formula:
CaAl2Si4O12 · 4H2O
Element Weights:
Other Information
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 Vanadio-laumontite
mindat.org URL:
https://www.mindat.org/min-4140.html
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References for Vanadio-laumontite
Localities for Vanadio-laumontite
Locality List
- 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).
All localities listed without proper references should be considered as questionable.
Kyrgyzstan | |
| Antipov et al. (1908) |
| Antipov et al. (1908) |
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