Number of the records: 1  

From mantle roots to surface eruptions: Cenozoic and Mesozoic continental basaltic magmatism

  1. 1.
    SYSNO ASEP0448855
    Document TypeJ - Journal Article
    R&D Document TypeThe record was not marked in the RIV
    Subsidiary JČlánek ve WOS
    TitleFrom mantle roots to surface eruptions: Cenozoic and Mesozoic continental basaltic magmatism
    Author(s) Kämpf, H. (DE)
    Németh, K. (NZ)
    Puziewicz, J. (PL)
    Mrlina, Jan (GFU-E) ORCID, RID
    Geissler, W.H. (DE)
    Source TitleInternational Journal of Earth Sciences. - : Springer - ISSN 1437-3254
    Roč. 104, č. 8 (2015), s. 1909-1912
    Number of pages4 s.
    Publication formPrint - P
    Languageeng - English
    CountryDE - Germany
    Keywordscontinental basaltic volcanism ; BASALT 2013 conference ; Cenozoic ; Mesozoic
    Subject RIVDC - Siesmology, Volcanology, Earth Structure
    Institutional supportGFU-E - RVO:67985530
    UT WOS000363871200001
    DOI10.1007/s00531-015-1252-5
    AnnotationBasaltic volcanism is an important process in shaping large areas of the Earth’s surface, not only in continental extensional environments and at the ocean floor. This special issue contains a collection of fifteen papers that are dedicated to recent researches on various aspects of continental basaltic magmatism from its mantle roots via the ascent paths of the melt to the surface where different styles of volcanism take place erupting lavas or through explosive volcanism depositing various types of pyroclasts. Two of the fifteen were published earlier. Continental basaltic volcanism also contributes to the total terrestrial sedimentary budget not only by its primary pyroclastic deposits but also their reworked varieties. Most of the papers result from presentations at the BASALT 2013 conference, which took place from April 18–24, 2013, in Görlitz.
    WorkplaceGeophysical Institute
    ContactHana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028
    Year of Publishing2016
Number of the records: 1  

  This site uses cookies to make them easier to browse. Learn more about how we use cookies.