Neogene and Quaternary rollback evolution of the Tyrrhenian Sea, the Apennines, and the Sicilian Maghrebides
Identifieur interne : 000471 ( Main/Exploration ); précédent : 000470; suivant : 000472Neogene and Quaternary rollback evolution of the Tyrrhenian Sea, the Apennines, and the Sicilian Maghrebides
Auteurs : Gideon Rosenbaum [Australie] ; Gordon S. Lister [Australie]Source :
- Tectonics [ 0278-7407 ] ; 2004-02.
Abstract
Reconstruction of the evolution of the Tyrrhenian Sea shows that the major stage of rifting associated with the opening of this basin began at ∼10 Ma. It involved two episodes of back arc extension, which were induced by the rollback of a west dipping subducting slab. The first period of extension (10–6 Ma) was prominent in the northern Tyrrhenian Sea and in the western part of the southern Tyrrhenian Sea. The second period of extension, mainly affected the southern Tyrrhenian Sea, began in the latest Messinian (6–5 Ma) and has been accompanied by subduction rollback at rates of 60–100 km Myr−1. Slab reconstruction, combined with paleomagnetic and paleogeographic constraints, indicates that in the central Apennines, the latest Messinian (6–5 Ma) arrival of a carbonate platform at the subduction zone impeded subduction and initiated a slab tear and major strike‐slip faults. These processes resulted in the formation of a narrow subducting slab beneath the Ionian Sea that has undergone faster subduction rollback and induced extreme rates of back arc extension.
Url:
DOI: 10.1029/2003TC001518
Affiliations:
Links toward previous steps (curation, corpus...)
- to stream Istex, to step Corpus: 000743
- to stream Istex, to step Curation: 000664
- to stream Istex, to step Checkpoint: 000438
- to stream Main, to step Merge: 000496
- to stream Main, to step Curation: 000491
Le document en format XML
<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title xml:lang="en">Neogene and Quaternary rollback evolution of the Tyrrhenian Sea, the Apennines, and the Sicilian Maghrebides</title><author><name sortKey="Rosenbaum, Gideon" sort="Rosenbaum, Gideon" uniqKey="Rosenbaum G" first="Gideon" last="Rosenbaum">Gideon Rosenbaum</name></author><author><name sortKey="Lister, Gordon S" sort="Lister, Gordon S" uniqKey="Lister G" first="Gordon S." last="Lister">Gordon S. Lister</name></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:6C0A985653F679E2EDF563A1D8337E0759EBA49D</idno><date when="2004" year="2004">2004</date><idno type="doi">10.1029/2003TC001518</idno><idno type="url">https://api.istex.fr/document/6C0A985653F679E2EDF563A1D8337E0759EBA49D/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">000743</idno><idno type="wicri:Area/Istex/Curation">000664</idno><idno type="wicri:Area/Istex/Checkpoint">000438</idno><idno type="wicri:doubleKey">0278-7407:2004:Rosenbaum G:neogene:and:quaternary</idno><idno type="wicri:Area/Main/Merge">000496</idno><idno type="wicri:Area/Main/Curation">000491</idno><idno type="wicri:Area/Main/Exploration">000471</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">Neogene and Quaternary rollback evolution of the Tyrrhenian Sea, the Apennines, and the Sicilian Maghrebides</title><author><name sortKey="Rosenbaum, Gideon" sort="Rosenbaum, Gideon" uniqKey="Rosenbaum G" first="Gideon" last="Rosenbaum">Gideon Rosenbaum</name><affiliation wicri:level="1"><country xml:lang="fr">Australie</country><wicri:regionArea>Australian Crustal Research Centre, School of Geosciences, Monash University, Victoria, Melbourne</wicri:regionArea><wicri:noRegion>Melbourne</wicri:noRegion></affiliation><affiliation wicri:level="1"><country wicri:rule="url">Australie</country></affiliation></author><author><name sortKey="Lister, Gordon S" sort="Lister, Gordon S" uniqKey="Lister G" first="Gordon S." last="Lister">Gordon S. Lister</name><affiliation wicri:level="1"><country xml:lang="fr">Australie</country><wicri:regionArea>Australian Crustal Research Centre, School of Geosciences, Monash University, Melbourne, Victoria</wicri:regionArea><wicri:noRegion>Victoria</wicri:noRegion></affiliation><affiliation wicri:level="1"><country xml:lang="fr" wicri:curation="lc">Australie</country><wicri:regionArea>Now at Research School of Earth Sciences, Australian National University, Canberra</wicri:regionArea><wicri:noRegion>Canberra</wicri:noRegion></affiliation></author></analytic><monogr></monogr><series><title level="j">Tectonics</title><title level="j" type="abbrev">Tectonics</title><idno type="ISSN">0278-7407</idno><idno type="eISSN">1944-9194</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><date type="published" when="2004-02">2004-02</date><biblScope unit="volume">23</biblScope><biblScope unit="issue">1</biblScope><biblScope unit="page" from="n/a">n/a</biblScope><biblScope unit="page" to="n/a">n/a</biblScope></imprint><idno type="ISSN">0278-7407</idno></series><idno type="istex">6C0A985653F679E2EDF563A1D8337E0759EBA49D</idno><idno type="DOI">10.1029/2003TC001518</idno><idno type="ArticleID">2003TC001518</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0278-7407</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract">Reconstruction of the evolution of the Tyrrhenian Sea shows that the major stage of rifting associated with the opening of this basin began at ∼10 Ma. It involved two episodes of back arc extension, which were induced by the rollback of a west dipping subducting slab. The first period of extension (10–6 Ma) was prominent in the northern Tyrrhenian Sea and in the western part of the southern Tyrrhenian Sea. The second period of extension, mainly affected the southern Tyrrhenian Sea, began in the latest Messinian (6–5 Ma) and has been accompanied by subduction rollback at rates of 60–100 km Myr−1. Slab reconstruction, combined with paleomagnetic and paleogeographic constraints, indicates that in the central Apennines, the latest Messinian (6–5 Ma) arrival of a carbonate platform at the subduction zone impeded subduction and initiated a slab tear and major strike‐slip faults. These processes resulted in the formation of a narrow subducting slab beneath the Ionian Sea that has undergone faster subduction rollback and induced extreme rates of back arc extension.</div></front></TEI><affiliations><list><country><li>Australie</li></country></list><tree><country name="Australie"><noRegion><name sortKey="Rosenbaum, Gideon" sort="Rosenbaum, Gideon" uniqKey="Rosenbaum G" first="Gideon" last="Rosenbaum">Gideon Rosenbaum</name></noRegion><name sortKey="Lister, Gordon S" sort="Lister, Gordon S" uniqKey="Lister G" first="Gordon S." last="Lister">Gordon S. Lister</name><name sortKey="Lister, Gordon S" sort="Lister, Gordon S" uniqKey="Lister G" first="Gordon S." last="Lister">Gordon S. Lister</name><name sortKey="Rosenbaum, Gideon" sort="Rosenbaum, Gideon" uniqKey="Rosenbaum G" first="Gideon" last="Rosenbaum">Gideon Rosenbaum</name></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
EXPLOR_STEP=$WICRI_ROOT/Wicri/Musique/explor/MonteverdiV1/Data/Main/Exploration
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 000471 | SxmlIndent | more
Ou
HfdSelect -h $EXPLOR_AREA/Data/Main/Exploration/biblio.hfd -nk 000471 | SxmlIndent | more
Pour mettre un lien sur cette page dans le réseau Wicri
{{Explor lien
|wiki= Wicri/Musique
|area= MonteverdiV1
|flux= Main
|étape= Exploration
|type= RBID
|clé= ISTEX:6C0A985653F679E2EDF563A1D8337E0759EBA49D
|texte= Neogene and Quaternary rollback evolution of the Tyrrhenian Sea, the Apennines, and the Sicilian Maghrebides
}}
| This area was generated with Dilib version V0.6.21. |  |