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Genesis of syntectonic hydrothermal veins in the igneous rock of teschenite association (Outer Western Carpathians, Czech Republic) : growth mechanism and origin of fluids

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F14%3A00080245" target="_blank" >RIV/00216224:14310/14:00080245 - isvavai.cz</a>

  • Result on the web

    <a href="http://www.geologicacarpathica.com/browse-journal/volumes/65-6/article-743/" target="_blank" >http://www.geologicacarpathica.com/browse-journal/volumes/65-6/article-743/</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1515/geoca-2015-003" target="_blank" >10.1515/geoca-2015-003</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Genesis of syntectonic hydrothermal veins in the igneous rock of teschenite association (Outer Western Carpathians, Czech Republic) : growth mechanism and origin of fluids

  • Original language description

    Hydrothermal mineralization hosted by the Lower Cretaceous igneous rock of the teschenite association at Jasenice (Silesian Unit, Flysch Belt, Outer Western Carpathians) occurs in two morphological types ? irregular vein filled by granular calcite and regular composite vein formed by both fibrous and granular calcite and minor chlorite, quartz, and pyrite. Crosscutting evidence indicates that the granular veins are younger than the composite vein. The composite vein was formed by two mechanisms at different times. The arrangement of solid inclusions in the marginal fibrous zone suggests an episodic growth by the crack-seal mechanism during syntectonic deformation which was at least partially driven by tectonic suction pump during some stages of the Alpine Orogeny. Both the central part of the composite vein and monomineral veins developed in a brittle regime. In these cases, the textures of vein suggest the flow of fluids along an open fracture.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    DB - Geology and mineralogy

  • OECD FORD branch

Result continuities

  • Project

  • Continuities

    S - Specificky vyzkum na vysokych skolach

Others

  • Publication year

    2014

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Geologica Carpathica

  • ISSN

    1336-8052

  • e-ISSN

  • Volume of the periodical

    65

  • Issue of the periodical within the volume

    prosinec 2014

  • Country of publishing house

    SK - SLOVAKIA

  • Number of pages

    13

  • Pages from-to

    419-431

  • UT code for WoS article

    000349683400003

  • EID of the result in the Scopus database