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.

Biostratigraphy and facies analysis of the Jatibungkus olistolith (Central Java)

Accordi G;Carbone F;
2010

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.
2010
Istituto di Geologia Ambientale e Geoingegneria - IGAG
Inglese
Forams 2010 - International Symposium on Foraminifera.
September 5-10, 2010
Bonn
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
2
info:eu-repo/semantics/conferenceObject
none
274
04 Contributo in convegno::04.02 Abstract in Atti di convegno
Accordi G.; Carbone F.; Di Carlo M.; Matteucci R.; Pignatti J.; Russo A.
File in questo prodotto:
Non ci sono file associati a questo prodotto.

I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.

Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/108514
Citazioni
  • ???jsp.display-item.citation.pmc??? ND
  • Scopus ND
  • ???jsp.display-item.citation.isi??? ND
social impact