The boundary of Larsen Basin on Tabarin Peninsula, Antarctica

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 b...

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Autores principales: del Valle, R.A., Scasso, R.A.
Formato: JOUR
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00044822_v59_n1_p38_delValle
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spelling todo:paper_00044822_v59_n1_p38_delValle2023-10-03T13:57:53Z The boundary of Larsen Basin on Tabarin Peninsula, Antarctica del Valle, R.A. Scasso, 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 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. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_00044822_v59_n1_p38_delValle
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
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
spellingShingle 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
del Valle, R.A.
Scasso, R.A.
The boundary of Larsen Basin on Tabarin Peninsula, Antarctica
topic_facet 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
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.
format JOUR
author del Valle, R.A.
Scasso, R.A.
author_facet del Valle, R.A.
Scasso, R.A.
author_sort del Valle, R.A.
title The boundary of Larsen Basin on Tabarin Peninsula, Antarctica
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 boundary of larsen basin on tabarin peninsula, antarctica
url http://hdl.handle.net/20.500.12110/paper_00044822_v59_n1_p38_delValle
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