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Bismuth and bismuth-antimony sulphosalts from Kutna Hora vein Ag-Pb-Zn ore district, Czech Republic

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60461373%3A22810%2F17%3A43913558" target="_blank" >RIV/60461373:22810/17:43913558 - isvavai.cz</a>

  • Alternative codes found

    RIV/00023272:_____/17:10133653 RIV/00025798:_____/17:00000168

  • Result on the web

    <a href="http://dx.doi.org/10.3190/jgeosci.230" target="_blank" >http://dx.doi.org/10.3190/jgeosci.230</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.3190/jgeosci.230" target="_blank" >10.3190/jgeosci.230</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Bismuth and bismuth-antimony sulphosalts from Kutna Hora vein Ag-Pb-Zn ore district, Czech Republic

  • Original language description

    A new, previously unknown association of Pb-Bi-Sb-Ag sulphosalt minerals has been found in samples from mine dumps of the Staroceske pasmo Lode of the Kutna flora Ag-Pb-Zn ore district, central Bohemia, Czech Republic. These minerals form polymirteral aggregates up to 1-3 cm in quartz or base sulphides. Apart from numerous members of lillianite homologous series, new occurrences of aramayoite, bismuthinite, cosalite, ikunolite, izoklakeite, matildite, galena,,, Bi-rich jamesonite, Bi-rich boulangerite, Bi-rich owyheeite and Bi-rich semseyite have been identified. An extraordinary extent of the Bi-Sb substitution is characteristic of the studied association. Bi-rich mineralization of this scope has not been previously known from the Kutna Hora ore district. The origin of this sulphosalt mineralization is related to the penetration of lower temperature fluids (c. 100-250 degrees C) into tectonically opened fractures in older ore veins filling. Virtually no mobilization of elements from the earlier vein filling took place; hydrothermal fluids must have been relatively rich in Ag and Ph and simultaneously poor in Cu. High Bi content was characteristic of the initial stage of the mineralization. Gradually, the Bi/Sb ratio decreased considerably with more Sb-rich minerals originating. At the final stage, Bi-rich Pb-Sb sulphosalts with lower A2 contents crystallized.

  • 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

    Result was created during the realization of more than one project. More information in the Projects tab.

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2017

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    JOURNAL OF GEOSCIENCES

  • ISSN

    1802-6222

  • e-ISSN

  • Volume of the periodical

    62

  • Issue of the periodical within the volume

    1

  • Country of publishing house

    CZ - CZECH REPUBLIC

  • Number of pages

    18

  • Pages from-to

    59-76

  • UT code for WoS article

    000400030700004

  • EID of the result in the Scopus database