Number of the records: 1  

Biostratigraphy of the Lower Cretaceous Schrambach Formation on the classical locality of Schrambachgraben (Northern Calcareous Alps, Salzburg Area)

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    SYSNO ASEP0439115
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleBiostratigraphy of the Lower Cretaceous Schrambach Formation on the classical locality of Schrambachgraben (Northern Calcareous Alps, Salzburg Area)
    Author(s) Boorová, D. (SK)
    Skupien, P. (CZ)
    Vašíček, Zdeněk (UGN-S) RID
    Number of authors3
    Source TitleBulletin of Geosciences. - : Česká geografická společnost - ISSN 1214-1119
    Roč. 90, č. 1 (2014), s. 89-131
    Number of pages43 s.
    Publication formOnline - E
    Languageeng - English
    CountryCZ - Czech Republic
    Keywordsbiostratigraphy ; Schrambach and Rossfeld formations ; Berriasian, Valanginian ; calcareous and non-calcareous dinoflagellata ; ammonites
    Subject RIVDB - Geology ; Mineralogy
    Institutional supportUGN-S - RVO:68145535
    UT WOS000348659800007
    EID SCOPUS2-s2.0-84982227969
    DOI10.3140/bull.geosci.1479
    AnnotationSchrambach Formation in the Eastern Alps area is conceived from the lithological and stratigraphical point of view rather non-uniform. Therefore a 200 m thick section in the type locality of the Schrambach Formation, situated south of Salzburg, is documented in this study. The studied sequence in the Schrambachgraben seems to be in the prevailing part of section in simple, monoclinal mode of deposition. The opposite is true. The section studied begins with the Oberalm Formation, passes gradually into the Schrambach Formation and ends with the lower part of the Rossfeld Formation. According to our detail results, deposits of the Schrambach Formation in this type of section occur in a minimum of three tectonic slices. The first tectonic slice is composed of a transitional sequence of the Oberalm Formation to the Schrambach Formation. The uppermost part of the Oberalm Formation is dated as the Middle Berriasian Calpionella Zone (Elliptica Subzone).
    WorkplaceInstitute of Geonics
    ContactLucie Gurková, lucie.gurkova@ugn.cas.cz, Tel.: 596 979 354
    Year of Publishing2015
    Electronic addresshttp://www.geology.cz/bulletin/fulltext/1479_Boorova_in_press.pdf
Number of the records: 1  

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