The boundary of Larsen Basin on Tabarin Peninsula, Antarctica
- Autores
- del Valle, R.A.; Scasso, R.A.
- Año de publicación
- 2004
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The Larsen Basin is the depositional area including all the upper Mesozoic-lower Cenozoic sedimentary rocks on the continental shelf of the northern Antarctic Peninsula. The western boundary between the basin fill and the rocks forming its technical basement, is not exposed, and was defined on the basis of aeromagnetic data. On petrological grounds, the Mesozoic marine sedimentary rocks exposed on western Tabarin Peninsula, at the north-eastern extremity of the Antarctic Peninsula, are assigned to the lower part of the Aptian-Eocene regressive megasequence that forms the basin filling. These rocks are faulted against sediments of the Antarctic Peninsula magmatic arc, suggesting that post- depositional tectonic movements probably occurred. This compressional deformation is assigned to mid-Cretaceous times, when the Coniacian partial basin inversion was accompanied by westward-verging deformation at the western basin margin. Although the original extent of the basin cannot be discerned from these data, the lithostratigraphical evidence and geographical position of the basin sediments, together with terrestrial magnetic data, confirm that the Larsen Basin extends onto the southern part of Tabarin Peninsula, and indicate that the western limit of the basin is located northward of the previously proposed limit. © 2004 Asociación Geológica Argentina.
Fil:del Valle, R.A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
Fil:Scasso, R.A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. - Fuente
- Rev. Asoc. Geol. Argent. 2004;59(1):38-44
- Materia
-
Early Cretaceous
Larsen Basin
Northern Antarctic Peninsula
Provenance
Stratigraphy
Tabarin Peninsula
basin fill
Cretaceous
depositional environment
provenance
regression
sequence stratigraphy
Antarctic Peninsula
Antarctica
Arctic and Antarctic
West Antarctica
World - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- http://creativecommons.org/licenses/by/2.5/ar
- Repositorio
.jpg)
- Institución
- Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturales
- OAI Identificador
- paperaa:paper_00044822_v59_n1_p38_delValle
Ver los metadatos del registro completo
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The boundary of Larsen Basin on Tabarin Peninsula, Antarctica del Valle, R.A.Scasso, R.A.Early CretaceousLarsen BasinNorthern Antarctic PeninsulaProvenanceStratigraphyTabarin Peninsulabasin fillCretaceousdepositional environmentprovenanceregressionsequence stratigraphyAntarctic PeninsulaAntarcticaArctic and AntarcticWest AntarcticaWorldThe Larsen Basin is the depositional area including all the upper Mesozoic-lower Cenozoic sedimentary rocks on the continental shelf of the northern Antarctic Peninsula. The western boundary between the basin fill and the rocks forming its technical basement, is not exposed, and was defined on the basis of aeromagnetic data. On petrological grounds, the Mesozoic marine sedimentary rocks exposed on western Tabarin Peninsula, at the north-eastern extremity of the Antarctic Peninsula, are assigned to the lower part of the Aptian-Eocene regressive megasequence that forms the basin filling. These rocks are faulted against sediments of the Antarctic Peninsula magmatic arc, suggesting that post- depositional tectonic movements probably occurred. This compressional deformation is assigned to mid-Cretaceous times, when the Coniacian partial basin inversion was accompanied by westward-verging deformation at the western basin margin. Although the original extent of the basin cannot be discerned from these data, the lithostratigraphical evidence and geographical position of the basin sediments, together with terrestrial magnetic data, confirm that the Larsen Basin extends onto the southern part of Tabarin Peninsula, and indicate that the western limit of the basin is located northward of the previously proposed limit. © 2004 Asociación Geológica Argentina.Fil:del Valle, R.A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.Fil:Scasso, R.A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.2004info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfhttp://hdl.handle.net/20.500.12110/paper_00044822_v59_n1_p38_delValleRev. Asoc. Geol. Argent. 2004;59(1):38-44reponame:Biblioteca Digital (UBA-FCEN)instname:Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturalesinstacron:UBA-FCENenginfo:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by/2.5/ar2026-02-05T12:42:53Zpaperaa:paper_00044822_v59_n1_p38_delValleInstitucionalhttps://digital.bl.fcen.uba.ar/Universidad públicaNo correspondehttps://digital.bl.fcen.uba.ar/cgi-bin/oaiserver.cgiana@bl.fcen.uba.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:18962026-02-05 12:42:54.704Biblioteca Digital (UBA-FCEN) - Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturalesfalse |
| dc.title.none.fl_str_mv |
The boundary of Larsen Basin on Tabarin Peninsula, Antarctica |
| title |
The boundary of Larsen Basin on Tabarin Peninsula, Antarctica |
| spellingShingle |
The boundary of Larsen Basin on Tabarin Peninsula, Antarctica del Valle, R.A. Early Cretaceous Larsen Basin Northern Antarctic Peninsula Provenance Stratigraphy Tabarin Peninsula basin fill Cretaceous depositional environment provenance regression sequence stratigraphy Antarctic Peninsula Antarctica Arctic and Antarctic West Antarctica World |
| title_short |
The boundary of Larsen Basin on Tabarin Peninsula, Antarctica |
| title_full |
The boundary of Larsen Basin on Tabarin Peninsula, Antarctica |
| title_fullStr |
The boundary of Larsen Basin on Tabarin Peninsula, Antarctica |
| title_full_unstemmed |
The boundary of Larsen Basin on Tabarin Peninsula, Antarctica |
| title_sort |
The boundary of Larsen Basin on Tabarin Peninsula, Antarctica |
| dc.creator.none.fl_str_mv |
del Valle, R.A. Scasso, R.A. |
| author |
del Valle, R.A. |
| author_facet |
del Valle, R.A. Scasso, R.A. |
| author_role |
author |
| author2 |
Scasso, R.A. |
| author2_role |
author |
| dc.subject.none.fl_str_mv |
Early Cretaceous Larsen Basin Northern Antarctic Peninsula Provenance Stratigraphy Tabarin Peninsula basin fill Cretaceous depositional environment provenance regression sequence stratigraphy Antarctic Peninsula Antarctica Arctic and Antarctic West Antarctica World |
| topic |
Early Cretaceous Larsen Basin Northern Antarctic Peninsula Provenance Stratigraphy Tabarin Peninsula basin fill Cretaceous depositional environment provenance regression sequence stratigraphy Antarctic Peninsula Antarctica Arctic and Antarctic West Antarctica World |
| dc.description.none.fl_txt_mv |
The Larsen Basin is the depositional area including all the upper Mesozoic-lower Cenozoic sedimentary rocks on the continental shelf of the northern Antarctic Peninsula. The western boundary between the basin fill and the rocks forming its technical basement, is not exposed, and was defined on the basis of aeromagnetic data. On petrological grounds, the Mesozoic marine sedimentary rocks exposed on western Tabarin Peninsula, at the north-eastern extremity of the Antarctic Peninsula, are assigned to the lower part of the Aptian-Eocene regressive megasequence that forms the basin filling. These rocks are faulted against sediments of the Antarctic Peninsula magmatic arc, suggesting that post- depositional tectonic movements probably occurred. This compressional deformation is assigned to mid-Cretaceous times, when the Coniacian partial basin inversion was accompanied by westward-verging deformation at the western basin margin. Although the original extent of the basin cannot be discerned from these data, the lithostratigraphical evidence and geographical position of the basin sediments, together with terrestrial magnetic data, confirm that the Larsen Basin extends onto the southern part of Tabarin Peninsula, and indicate that the western limit of the basin is located northward of the previously proposed limit. © 2004 Asociación Geológica Argentina. Fil:del Valle, R.A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Scasso, R.A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. |
| description |
The Larsen Basin is the depositional area including all the upper Mesozoic-lower Cenozoic sedimentary rocks on the continental shelf of the northern Antarctic Peninsula. The western boundary between the basin fill and the rocks forming its technical basement, is not exposed, and was defined on the basis of aeromagnetic data. On petrological grounds, the Mesozoic marine sedimentary rocks exposed on western Tabarin Peninsula, at the north-eastern extremity of the Antarctic Peninsula, are assigned to the lower part of the Aptian-Eocene regressive megasequence that forms the basin filling. These rocks are faulted against sediments of the Antarctic Peninsula magmatic arc, suggesting that post- depositional tectonic movements probably occurred. This compressional deformation is assigned to mid-Cretaceous times, when the Coniacian partial basin inversion was accompanied by westward-verging deformation at the western basin margin. Although the original extent of the basin cannot be discerned from these data, the lithostratigraphical evidence and geographical position of the basin sediments, together with terrestrial magnetic data, confirm that the Larsen Basin extends onto the southern part of Tabarin Peninsula, and indicate that the western limit of the basin is located northward of the previously proposed limit. © 2004 Asociación Geológica Argentina. |
| publishDate |
2004 |
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2004 |
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info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
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article |
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publishedVersion |
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http://hdl.handle.net/20.500.12110/paper_00044822_v59_n1_p38_delValle |
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http://hdl.handle.net/20.500.12110/paper_00044822_v59_n1_p38_delValle |
| dc.language.none.fl_str_mv |
eng |
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eng |
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info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar |
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openAccess |
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http://creativecommons.org/licenses/by/2.5/ar |
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application/pdf |
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