Smamite, Ca2Sb(OH)4[H(AsO4)2] • 6H2O, a new mineral and a possible sink for Sb during weathering of fahlore

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68378271%3A_____%2F20%3A00537724" target="_blank" >RIV/68378271:_____/20:00537724 - isvavai.cz</a>
Result on the web
<a href="https://doi.org/10.2138/am-2020-7133" target="_blank" >https://doi.org/10.2138/am-2020-7133</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.2138/am-2020-7133" target="_blank" >10.2138/am-2020-7133</a>

Result language
angličtina
Original language name
Smamite, Ca2Sb(OH)4[H(AsO4)2] • 6H2O, a new mineral and a possible sink for Sb during weathering of fahlore
Original language description
Smamite, Ca2Sb(OH)4[H(AsO4)2]•6H2O, is a new mineral species from the Giftgrube mine, Rauenthal, Sainte-Marie-Aux-Mines ore-district, Haut-Rhin department, France. It is a supergene mineral found in quartz-carbonate gangue with disseminated to massive tennantite-tetrahedrite series minerals, native arsenic, Ni-Co arsenides, and supergene minerals picropharmacolite, fluckite, and pharmacolite. Smamite occurs as lenticular crystals growing in aggregates up to 0.5mm across. in this work tme mineral's structure and its properties were studied and the results are presented.n
Czech name
—
Czech description
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Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
—
OECD FORD branch
10504 - Mineralogy

Project
<a href="/en/project/GA17-09161S" target="_blank" >GA17-09161S: Crystal structures, chemistry and stability of arsenate and sulfate minerals</a><br>
Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Publication year
2020
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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