Biostratigraphy and facies analysis of the Jatibungkus olistolith (Central Java) (Abstract/Poster in atti di convegno)

Type
Label
  • Biostratigraphy and facies analysis of the Jatibungkus olistolith (Central Java) (Abstract/Poster in atti di convegno) (literal)
Anno
  • 2010-01-01T00:00:00+01:00 (literal)
Alternative label
  • Accordi G.; Carbone F.; Di Carlo M.; Matteucci R.; Pignatti J.; Russo A. (2010)
    Biostratigraphy and facies analysis of the Jatibungkus olistolith (Central Java)
    in Forams 2010 - International Symposium on Foraminifera., Bonn, September 5-10, 2010
    (literal)
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  • Accordi G.; Carbone F.; Di Carlo M.; Matteucci R.; Pignatti J.; Russo A. (literal)
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  • Titolo del volume degli abstracts: FORAMS 2010 - International Symposium on Foraminifera : Abstracts Volume with Program. Core Organizing Committee: Martin Langer; Anna Weinmann; Beate Söntgerath; Peter Göddertz; Georg Heumann (literal)
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  • Rheinische Friedrich-Wilhelms-Universität Bonn, September 5-10, 2010, Germany. Poster presentation. (literal)
Note
  • Abstract (literal)
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  • Accordi Giovanni - Istituto di Geologia Ambientale e Geoingegneria Carbone Federico - Istituto di Geologia Ambientale e Geoingegneria (literal)
Titolo
  • Biostratigraphy and facies analysis of the Jatibungkus olistolith (Central Java) (literal)
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  • Martin Langer; Anna Weinmann; Beate Söntgerath; Peter Göddertz; Georg Heumann (literal)
Abstract
  • The Eocene Karangsambung Olistostrome (or mélange) contains numerous blocks of different sedimentary, volcanic and metamorphic rocks, up to several hundreds meters in diameter; among these olistoliths, we investigate the fossil content, sedimentology, facies interpretation and age assignment of the huge Jatibungkus limestone olistolith, which has been subject to contrasting interpretations. Basing on larger foraminifers (Ranikothalia, Miscellanea, rotaliids, and orthophragmines), scleractinians (11 species belonging to 9 genera) and calcareous algae, the Jatibungkus limestone can be broadly considered as Thanetian in age (SBZ3/SBZ4). On the base of thin sections, the taxonomy of the larger foraminifers is discussed in detail, attempting to constrain and extend to this area the Shallow Benthics Zonation. Basing on sedimentological data, the occurrence and growth forms of Distichoplax biserialis, the scleractinian and larger foraminiferal assemblages allow us to identify three main depositional environments. (literal)
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