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Crystal structure of Pb-bearing watanabeite from Pefka, Greece

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00023272%3A_____%2F24%3A10136678" target="_blank" >RIV/00023272:_____/24:10136678 - isvavai.cz</a>

  • Result on the web

    <a href="https://www.cambridge.org/core/journals/mineralogical-magazine/article/crystal-structure-of-pbbearing-watanabeite-from-pefka-greece/18921585318E0FE9322BBA29ED87017B" target="_blank" >https://www.cambridge.org/core/journals/mineralogical-magazine/article/crystal-structure-of-pbbearing-watanabeite-from-pefka-greece/18921585318E0FE9322BBA29ED87017B</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1180/mgm.2024.14" target="_blank" >10.1180/mgm.2024.14</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Crystal structure of Pb-bearing watanabeite from Pefka, Greece

  • Original language description

    Watanabeite from the Pefka epithermal deposit, northeastern Greece, was examined using single-crystal X-ray diffraction and electron microprobe analysis. Empirical formula of watanabeite is Cu3.93Fe0.10Ag0.01Pb0.23(As1.55Sb0.19)Σ1.74S4.99. This mineral is orthorhombic, space group Amm2, with unit-cell parameters a = 10.9601(5), b = 14.6498(8), c = 10.3001(5) Å, V = 1653.82(14) Å3, Z = 8. The crystal structure was solved and refined to R1 = 0.0471 for 2108 unique reflections with Fo &gt; 4σ(Fo) and 123 refined parameters. The crystal structure of watanabeite can be described as a three-dimensional framework of Cu-centered tetrahedra; cavities of the tetrahedral scaffolding host Cu6S and As2(Pb,Sb,As)2S7 clusters. On the basis of structural data, the formula of watanabeite could be written as [III]Cu3[IV]Cu5As3(Pb,Sb,As)S10 (Z = 4), considering the three independent three-fold Cu sites and the three independent tetrahedrally coordinated Cu sites as aggregated positions. The occurrence of Pb2+ in watanabeite is probably related to the substitution Cu+ + (As,Sb)3+ = 2Me2+, where Me = Pb, Fe, Zn, and formally divalent Cu. The relations with tetrahedrite-group minerals are discussed on the basis of the refined structural model, highlighting possible crystal chemical implications of such relationships.

  • Czech name

  • Czech description

Classification

  • 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

Result continuities

  • Project

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2024

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Mineralogical Magazine

  • ISSN

    0026-461X

  • e-ISSN

  • Volume of the periodical

    88

  • Issue of the periodical within the volume

    3

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    10

  • Pages from-to

    218-227

  • UT code for WoS article

    001204498500001

  • EID of the result in the Scopus database