Record details

Title
    The origin and mineralization of the tin-bearing granites of the Krušné hory (Erzgebirge) province: A 3-dimensional approach with new data on ore deposit zoning around a granite batholith
Statement of responsibility
    Miroslav Štemprok
Other titles
    Deep Structure of the Earth and Concentration of Metals in the Lithosphere: A Geodynamic Approach (Variant.)
Author
    Štemprok, Miroslav
Language
    anglicky
Source title - serial
    Global tectonics and metallogeny
Vol./nr.
    Vol. 8, no. 1-4
Pages
    p. 215-226
Year
    2003
Notes
    3 obr., 2 tab., 2 s. bibl.
    il.
    Zkr. název ser.: Glob. Tecton. Metallog.
Subject group
    anomálie tíhová
    batolit
    diskontinuita Mohorovičičova
    granit
    krušnohorské krystalinikum
    krušnohorský pluton
    ložisko barytu
    ložisko fluoritu
    provincie metalogenetická
    rudy Ag
    rudy barevných kovů
    rudy Fe
    rudy Sn
    rudy U
    rudy W
    vrásnění variské
    zdroje zrudnění
    zonálnost
    zonálnost mineralizace
Geographical name
    Cínovec (Teplice)
    ČR-Čechy
    Jáchymov (Karlovy Vary)
    Kovářská (Chomutov)
    Krásno (Sokolov)
    Krupka (Teplice)
    Měděnec (Chomutov)
    Moldava (Teplice)
    Přebuz (Sokolov)
    Rolava (Karlovy Vary)
    SRN-Sachsen
    Telnice (Ústí nad Labem)
    Tisová (Sokolov)
Keyword
    3-dimensional
    Approach
    Around
    Batholith
    Data
    Deposit
    Erzgebirge
    Granite
    Granites
    Hory
    Krušné
    Mineralization
    New
    Ore
    Origin
    Province
    Tin-bearing
    Zoning
Abstract (in english)
   The new summary of metallogeny of the Erzgebirge/Krušné hory granite batholith (Sn, W, U, Pb-Zn, Ag, Bi, Co, Ni, fluorite and barite) in Central Europe shows that the symmetrical and synchronous mineral zones around the granitic magmatic foci of temperature and pressure do not exist. The irregular distribution of mineral districts is controlled by the lines of emplacement of younger (YIC) granites, by major deep-seated fault zones and by the local lithology in the envelope. Variously mineralized crustal segments were exposed to different fluids of various origin after the emplacement of granites. This is the main cause for the irregular distribution of orebearing assemblages in relation to the granites which early workers interpreted as horizontal mineral zoning
Contributor
    Česká geologická služba
Contributor code
    ČGS (UNM)
Source format
    U
Entered date
    1. 10. 2007
Import date
    8. 8. 2012