The crystal structure of franckeite, Pb21.7Sn9.3Fe4.0Sb8.1S56.9.
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68378271%3A_____%2F11%3A00371134" target="_blank" >RIV/68378271:_____/11:00371134 - isvavai.cz</a>
Result on the web
<a href="http://dx.doi.org/10.2138/am.2011.3814" target="_blank" >http://dx.doi.org/10.2138/am.2011.3814</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.2138/am.2011.3814" target="_blank" >10.2138/am.2011.3814</a>
Alternative languages
Result language
angličtina
Original language name
The crystal structure of franckeite, Pb21.7Sn9.3Fe4.0Sb8.1S56.9.
Original language description
The layer-like crystal structure of franckeite exhibits a pronounced one-dimensional transversal wave-like modulation and a non-commensurate layer match in two dimensions. It consists of alternating pseudohexagonal (H) layers and pseudotetragonal (Q) slabs and forms a homologous pair with cylindrite, which has thinner Q slabs. The Q slabs in franckeite are four atomic layers thick. The two components have their own lattices and a common modulation.
Czech name
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Czech description
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Classification
Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
BM - Solid-state physics and magnetism
OECD FORD branch
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Result continuities
Project
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Continuities
Z - Vyzkumny zamer (s odkazem do CEZ)
Others
Publication year
2011
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
American Mineralogist
ISSN
0003-004X
e-ISSN
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Volume of the periodical
96
Issue of the periodical within the volume
11
Country of publishing house
US - UNITED STATES
Number of pages
17
Pages from-to
1686-1702
UT code for WoS article
000297241400003
EID of the result in the Scopus database
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