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Distribution and origin of clay minerals during hydrothermal alteration of ore deposits

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985891%3A_____%2F12%3A00380469" target="_blank" >RIV/67985891:_____/12:00380469 - isvavai.cz</a>

  • Result on the web

    <a href="http://dx.doi.org/10.5772/48312" target="_blank" >http://dx.doi.org/10.5772/48312</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.5772/48312" target="_blank" >10.5772/48312</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Distribution and origin of clay minerals during hydrothermal alteration of ore deposits

  • Original language description

    Hydrothermal alterations of host rocks (granites and metasediments) connected with origin ore deposits are often accompanied by origin of clay minerals. In area of the Bohemian Massif occur a few Sn-W- and U-ore deposits in which are evolved alteration zones with highly interested clay minerals assemblage.

  • Czech name

  • Czech description

Classification

  • Type

    C - Chapter in a specialist book

  • CEP classification

    DB - Geology and mineralogy

  • OECD FORD branch

Result continuities

  • Project

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

  • Continuities

    Z - Vyzkumny zamer (s odkazem do CEZ)

Others

  • Publication year

    2012

  • Confidentiality

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

Data specific for result type

  • Book/collection name

    Clay Minerals in Nature ? Their characterization, modification and application

  • ISBN

    9789535107385

  • Number of pages of the result

    20

  • Pages from-to

    81-100

  • Number of pages of the book

    312

  • Publisher name

    Intech

  • Place of publication

    Rijeka

  • UT code for WoS chapter