All

What are you looking for?

All
Projects
Results
Organizations

Quick search

  • Projects supported by TA ČR
  • Excellent projects
  • Projects with the highest public support
  • Current projects

Smart search

  • That is how I find a specific +word
  • That is how I leave the -word out of the results
  • “That is how I can find the whole phrase”

Neoproterozoic to early Cambrian Franciscan-type mélanges in the Teplá-Barrandian unit, Bohemian Massif: Evidence of modern-style accretionary processes along the Cadomian active margin of Gondwana?

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F13%3A10173867" target="_blank" >RIV/00216208:11310/13:10173867 - isvavai.cz</a>

  • Result on the web

    <a href="http://dx.doi.org/10.1016/j.precamres.2012.11.007" target="_blank" >http://dx.doi.org/10.1016/j.precamres.2012.11.007</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.precamres.2012.11.007" target="_blank" >10.1016/j.precamres.2012.11.007</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Neoproterozoic to early Cambrian Franciscan-type mélanges in the Teplá-Barrandian unit, Bohemian Massif: Evidence of modern-style accretionary processes along the Cadomian active margin of Gondwana?

  • Original language description

    Mélanges have been reported from a variety of modern tectonic settings and are a hallmark of the Franciscan-type subduction-accretion complexes. In the Precambrian, however, well documented examples of melanges become extremely scarce. This paper describes in detail Neoproterozoic to early Cambrian melanges recently recognized in the Cadomian basement of the Teplá-Barrandian unit, Bohemian Massif. The melanges are of sedimentary and tectonic origin and include voluminous successions of graywackes interpreted to represent mass-transport deposits presumably along the upper slope of an accretionary wedge. The clast compositions indicate multiple episodes of mixing of terrigenous arc-derived and deep-water (?pelagic) material. Moreover, abundant bodies of(meta-)basalts, interpreted as dismembered seamounts or pillow volcanoes, were emplaced tectonically into various structural levels of this sedimentary melange by two different mechanisms. At an upper level, the irregular to elongated bod

  • 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

    Z - Vyzkumny zamer (s odkazem do CEZ)<br>S - Specificky vyzkum na vysokych skolach<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2013

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Precambrian Research

  • ISSN

    0301-9268

  • e-ISSN

  • Volume of the periodical

    224

  • Issue of the periodical within the volume

    leden

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    18

  • Pages from-to

    653-670

  • UT code for WoS article

    000313765800037

  • EID of the result in the Scopus database