The detrital zircon record of Variscan to post‑Variscan tectonosedimentary and magmatic processes in the Tauern Window (Eastern Alps)

Autores
Veselá, P.; Oriolo, Sebastián; Basei, M. A. S.; Lammerer, Bernd; Siegesmund, S.
Año de publicación
2022
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Coupled U–Pb and Lu–Hf LA-ICP-MS detrital and igneous zircon data were obtained from metasedimentary sequences (Kaserer Formation, Schmirntal Quartzite, Seidlwinkel Formation, Bündnerschiefer Basin, Riffler Basin) of the western Tauern Window (Eastern Alps). Results show maximum deposition ages between the Late Permian and the Triassic, indicating protracted sedimentation and magmatism between the Late Paleozoic and the Mesozoic. The Lu–Hf fingerprint shows a change from subchondritic to variable subchondritic to suprachondritic compositions at ca. 290 Ma, possibly documenting the transition from Late Paleozoic Variscan post-collisional processes to intracontinental extension. Lithospheric thinning and magmatic underplating may explain the observed Hf isotopic evolution as the result of mixing of crustal and mantellic sources. From a paleogeographical perspective, results confirm that the Tauern Window was situated between Alpine basement units (South Alpine, Austroalpine and External Massifs) and the Bohemian Massif during the Permian–Triassic.
Fil: Veselá, P.. Ludwig Maximilians Universitat; Alemania
Fil: Oriolo, Sebastián. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; Argentina
Fil: Basei, M. A. S.. Universidade de Sao Paulo; Brasil
Fil: Lammerer, Bernd. Ludwig Maximilians Universitat; Alemania
Fil: Siegesmund, S.. Universität Göttingen; Alemania
Materia
ALPINE BASEMENT
LU–HF ISOTOPES
PANGEA BREAK-UP
PENNINIC OCEAN
PERMIAN–TRIASSIC INTRACONTINENTAL RIFTING
VARISCAN OROGENY
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/202811
Acceder
id CONICETDig_813cce2728a33ac61c43eb8525a32c0b
oai_identifier_str oai:ri.conicet.gov.ar:11336/202811
network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling The detrital zircon record of Variscan to post‑Variscan tectonosedimentary and magmatic processes in the Tauern Window (Eastern Alps)Veselá, P.Oriolo, SebastiánBasei, M. A. S.Lammerer, BerndSiegesmund, S.ALPINE BASEMENTLU–HF ISOTOPESPANGEA BREAK-UPPENNINIC OCEANPERMIAN–TRIASSIC INTRACONTINENTAL RIFTINGVARISCAN OROGENYhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Coupled U–Pb and Lu–Hf LA-ICP-MS detrital and igneous zircon data were obtained from metasedimentary sequences (Kaserer Formation, Schmirntal Quartzite, Seidlwinkel Formation, Bündnerschiefer Basin, Riffler Basin) of the western Tauern Window (Eastern Alps). Results show maximum deposition ages between the Late Permian and the Triassic, indicating protracted sedimentation and magmatism between the Late Paleozoic and the Mesozoic. The Lu–Hf fingerprint shows a change from subchondritic to variable subchondritic to suprachondritic compositions at ca. 290 Ma, possibly documenting the transition from Late Paleozoic Variscan post-collisional processes to intracontinental extension. Lithospheric thinning and magmatic underplating may explain the observed Hf isotopic evolution as the result of mixing of crustal and mantellic sources. From a paleogeographical perspective, results confirm that the Tauern Window was situated between Alpine basement units (South Alpine, Austroalpine and External Massifs) and the Bohemian Massif during the Permian–Triassic.Fil: Veselá, P.. Ludwig Maximilians Universitat; AlemaniaFil: Oriolo, Sebastián. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; ArgentinaFil: Basei, M. A. S.. Universidade de Sao Paulo; BrasilFil: Lammerer, Bernd. Ludwig Maximilians Universitat; AlemaniaFil: Siegesmund, S.. Universität Göttingen; AlemaniaSpringer2022-03-19info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/202811Veselá, P.; Oriolo, Sebastián; Basei, M. A. S.; Lammerer, Bernd; Siegesmund, S.; The detrital zircon record of Variscan to post‑Variscan tectonosedimentary and magmatic processes in the Tauern Window (Eastern Alps); Springer; International Journal of Earth Sciences; 111; 4; 19-3-2022; 1273-12871437-3254CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1007/s00531-022-02179-0info:eu-repo/semantics/altIdentifier/url/https://link.springer.com/article/10.1007/s00531-022-02179-0info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:29:34Zoai:ri.conicet.gov.ar:11336/202811instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 10:29:35.04CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv The detrital zircon record of Variscan to post‑Variscan tectonosedimentary and magmatic processes in the Tauern Window (Eastern Alps)
title The detrital zircon record of Variscan to post‑Variscan tectonosedimentary and magmatic processes in the Tauern Window (Eastern Alps)
spellingShingle The detrital zircon record of Variscan to post‑Variscan tectonosedimentary and magmatic processes in the Tauern Window (Eastern Alps)
Veselá, P.
ALPINE BASEMENT
LU–HF ISOTOPES
PANGEA BREAK-UP
PENNINIC OCEAN
PERMIAN–TRIASSIC INTRACONTINENTAL RIFTING
VARISCAN OROGENY
title_short The detrital zircon record of Variscan to post‑Variscan tectonosedimentary and magmatic processes in the Tauern Window (Eastern Alps)
title_full The detrital zircon record of Variscan to post‑Variscan tectonosedimentary and magmatic processes in the Tauern Window (Eastern Alps)
title_fullStr The detrital zircon record of Variscan to post‑Variscan tectonosedimentary and magmatic processes in the Tauern Window (Eastern Alps)
title_full_unstemmed The detrital zircon record of Variscan to post‑Variscan tectonosedimentary and magmatic processes in the Tauern Window (Eastern Alps)
title_sort The detrital zircon record of Variscan to post‑Variscan tectonosedimentary and magmatic processes in the Tauern Window (Eastern Alps)
dc.creator.none.fl_str_mv Veselá, P.
Oriolo, Sebastián
Basei, M. A. S.
Lammerer, Bernd
Siegesmund, S.
author Veselá, P.
author_facet Veselá, P.
Oriolo, Sebastián
Basei, M. A. S.
Lammerer, Bernd
Siegesmund, S.
author_role author
author2 Oriolo, Sebastián
Basei, M. A. S.
Lammerer, Bernd
Siegesmund, S.
author2_role author
author
author
author
dc.subject.none.fl_str_mv ALPINE BASEMENT
LU–HF ISOTOPES
PANGEA BREAK-UP
PENNINIC OCEAN
PERMIAN–TRIASSIC INTRACONTINENTAL RIFTING
VARISCAN OROGENY
topic ALPINE BASEMENT
LU–HF ISOTOPES
PANGEA BREAK-UP
PENNINIC OCEAN
PERMIAN–TRIASSIC INTRACONTINENTAL RIFTING
VARISCAN OROGENY
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Coupled U–Pb and Lu–Hf LA-ICP-MS detrital and igneous zircon data were obtained from metasedimentary sequences (Kaserer Formation, Schmirntal Quartzite, Seidlwinkel Formation, Bündnerschiefer Basin, Riffler Basin) of the western Tauern Window (Eastern Alps). Results show maximum deposition ages between the Late Permian and the Triassic, indicating protracted sedimentation and magmatism between the Late Paleozoic and the Mesozoic. The Lu–Hf fingerprint shows a change from subchondritic to variable subchondritic to suprachondritic compositions at ca. 290 Ma, possibly documenting the transition from Late Paleozoic Variscan post-collisional processes to intracontinental extension. Lithospheric thinning and magmatic underplating may explain the observed Hf isotopic evolution as the result of mixing of crustal and mantellic sources. From a paleogeographical perspective, results confirm that the Tauern Window was situated between Alpine basement units (South Alpine, Austroalpine and External Massifs) and the Bohemian Massif during the Permian–Triassic.
Fil: Veselá, P.. Ludwig Maximilians Universitat; Alemania
Fil: Oriolo, Sebastián. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; Argentina
Fil: Basei, M. A. S.. Universidade de Sao Paulo; Brasil
Fil: Lammerer, Bernd. Ludwig Maximilians Universitat; Alemania
Fil: Siegesmund, S.. Universität Göttingen; Alemania
description Coupled U–Pb and Lu–Hf LA-ICP-MS detrital and igneous zircon data were obtained from metasedimentary sequences (Kaserer Formation, Schmirntal Quartzite, Seidlwinkel Formation, Bündnerschiefer Basin, Riffler Basin) of the western Tauern Window (Eastern Alps). Results show maximum deposition ages between the Late Permian and the Triassic, indicating protracted sedimentation and magmatism between the Late Paleozoic and the Mesozoic. The Lu–Hf fingerprint shows a change from subchondritic to variable subchondritic to suprachondritic compositions at ca. 290 Ma, possibly documenting the transition from Late Paleozoic Variscan post-collisional processes to intracontinental extension. Lithospheric thinning and magmatic underplating may explain the observed Hf isotopic evolution as the result of mixing of crustal and mantellic sources. From a paleogeographical perspective, results confirm that the Tauern Window was situated between Alpine basement units (South Alpine, Austroalpine and External Massifs) and the Bohemian Massif during the Permian–Triassic.
publishDate 2022
dc.date.none.fl_str_mv 2022-03-19
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/202811
Veselá, P.; Oriolo, Sebastián; Basei, M. A. S.; Lammerer, Bernd; Siegesmund, S.; The detrital zircon record of Variscan to post‑Variscan tectonosedimentary and magmatic processes in the Tauern Window (Eastern Alps); Springer; International Journal of Earth Sciences; 111; 4; 19-3-2022; 1273-1287
1437-3254
CONICET Digital
CONICET
url http://hdl.handle.net/11336/202811
identifier_str_mv Veselá, P.; Oriolo, Sebastián; Basei, M. A. S.; Lammerer, Bernd; Siegesmund, S.; The detrital zircon record of Variscan to post‑Variscan tectonosedimentary and magmatic processes in the Tauern Window (Eastern Alps); Springer; International Journal of Earth Sciences; 111; 4; 19-3-2022; 1273-1287
1437-3254
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1007/s00531-022-02179-0
info:eu-repo/semantics/altIdentifier/url/https://link.springer.com/article/10.1007/s00531-022-02179-0
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Springer
publisher.none.fl_str_mv Springer
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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score 13.070432

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