Late Cretaceous paleogeography of the Antarctic Peninsula: New paleomagnetic pole from the James Ross Basin

Two paleomagnetic poles of 80 and 75 Ma have been computed from 191 to 123 paleomagnetic samples, respectively, of the marine sedimentary units of the Upper Cretaceous Marambio Group exposed in the James Ross Island, Antarctic Peninsula. Paleomagnetic behaviors during stepwise thermal demagnetizatio...

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Autores principales: Milanese, F., Rapalini, A., Slotznick, S.P., Tobin, T.S., Kirschvink, J., Olivero, E.
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_08959811_v91_n_p131_Milanese
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spelling todo:paper_08959811_v91_n_p131_Milanese2023-10-03T15:43:43Z Late Cretaceous paleogeography of the Antarctic Peninsula: New paleomagnetic pole from the James Ross Basin Milanese, F. Rapalini, A. Slotznick, S.P. Tobin, T.S. Kirschvink, J. Olivero, E. Apparent polar wander path Gustav group Marambio group Paleomagnetism apparent polar wander path Cretaceous magnetic field magnetization paleogeography paleomagnetism Antarctic Peninsula Antarctica James Ross Island West Antarctica Two paleomagnetic poles of 80 and 75 Ma have been computed from 191 to 123 paleomagnetic samples, respectively, of the marine sedimentary units of the Upper Cretaceous Marambio Group exposed in the James Ross Island, Antarctic Peninsula. Paleomagnetic behaviors during stepwise thermal demagnetization and rock magnetic analyses indicate that magnetization is likely primary and carried by SD-PSD detrital titanomagnetite. Application of an inclination shallowing correction by the elongation-inclination method yielded a significant inclination shallowing affecting the older (ca. 80 Ma) succession exposed in the northwest area of the island. However, the paleomagnetic directions computed from the younger (ca. 75 Ma) succession outcropping in the southeast corner of the island yielded an indeterminate result using the same analysis. The inclination shallowing-corrected 80 Ma paleopole position plus previous ones of ca.110, 90 and 55 Ma were used to construct the Apparent Polar Wander Path (APWP) for the Antarctic Peninsula during the Late Cretaceous-Paleocene. This path confirms that oroclinal bending of the Antarctic Peninsula as well as relative displacement with respect to East Antarctica are negligible since 110 Ma. Comparison with the apparent polar wander path for South America for the 130-45 Ma period suggests that this continent and the Antarctic Peninsula kept a very similar relative paleogeographic position since 110 Ma until 55 Ma, which likely meant a physical link between both continental masses. During that period, both continents underwent a relatively fast southward displacement of around 7° and a clockwise rotation relative to the Earth spin axis that can be bracketed between around 100 and 90 Ma. Oroclinal bending of the Fuegian Andes was likely due to tectonic interactions between the Patagonian-Fuegian Andes and the Antarctic Peninsula promoted, at least partially, by such displacements. By 55 Ma the Antarctic Peninsula probably was starting or about to start its final separation from South America. © 2019 Elsevier Ltd JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_08959811_v91_n_p131_Milanese
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Apparent polar wander path
Gustav group
Marambio group
Paleomagnetism
apparent polar wander path
Cretaceous
magnetic field
magnetization
paleogeography
paleomagnetism
Antarctic Peninsula
Antarctica
James Ross Island
West Antarctica
spellingShingle Apparent polar wander path
Gustav group
Marambio group
Paleomagnetism
apparent polar wander path
Cretaceous
magnetic field
magnetization
paleogeography
paleomagnetism
Antarctic Peninsula
Antarctica
James Ross Island
West Antarctica
Milanese, F.
Rapalini, A.
Slotznick, S.P.
Tobin, T.S.
Kirschvink, J.
Olivero, E.
Late Cretaceous paleogeography of the Antarctic Peninsula: New paleomagnetic pole from the James Ross Basin
topic_facet Apparent polar wander path
Gustav group
Marambio group
Paleomagnetism
apparent polar wander path
Cretaceous
magnetic field
magnetization
paleogeography
paleomagnetism
Antarctic Peninsula
Antarctica
James Ross Island
West Antarctica
description Two paleomagnetic poles of 80 and 75 Ma have been computed from 191 to 123 paleomagnetic samples, respectively, of the marine sedimentary units of the Upper Cretaceous Marambio Group exposed in the James Ross Island, Antarctic Peninsula. Paleomagnetic behaviors during stepwise thermal demagnetization and rock magnetic analyses indicate that magnetization is likely primary and carried by SD-PSD detrital titanomagnetite. Application of an inclination shallowing correction by the elongation-inclination method yielded a significant inclination shallowing affecting the older (ca. 80 Ma) succession exposed in the northwest area of the island. However, the paleomagnetic directions computed from the younger (ca. 75 Ma) succession outcropping in the southeast corner of the island yielded an indeterminate result using the same analysis. The inclination shallowing-corrected 80 Ma paleopole position plus previous ones of ca.110, 90 and 55 Ma were used to construct the Apparent Polar Wander Path (APWP) for the Antarctic Peninsula during the Late Cretaceous-Paleocene. This path confirms that oroclinal bending of the Antarctic Peninsula as well as relative displacement with respect to East Antarctica are negligible since 110 Ma. Comparison with the apparent polar wander path for South America for the 130-45 Ma period suggests that this continent and the Antarctic Peninsula kept a very similar relative paleogeographic position since 110 Ma until 55 Ma, which likely meant a physical link between both continental masses. During that period, both continents underwent a relatively fast southward displacement of around 7° and a clockwise rotation relative to the Earth spin axis that can be bracketed between around 100 and 90 Ma. Oroclinal bending of the Fuegian Andes was likely due to tectonic interactions between the Patagonian-Fuegian Andes and the Antarctic Peninsula promoted, at least partially, by such displacements. By 55 Ma the Antarctic Peninsula probably was starting or about to start its final separation from South America. © 2019 Elsevier Ltd
format JOUR
author Milanese, F.
Rapalini, A.
Slotznick, S.P.
Tobin, T.S.
Kirschvink, J.
Olivero, E.
author_facet Milanese, F.
Rapalini, A.
Slotznick, S.P.
Tobin, T.S.
Kirschvink, J.
Olivero, E.
author_sort Milanese, F.
title Late Cretaceous paleogeography of the Antarctic Peninsula: New paleomagnetic pole from the James Ross Basin
title_short Late Cretaceous paleogeography of the Antarctic Peninsula: New paleomagnetic pole from the James Ross Basin
title_full Late Cretaceous paleogeography of the Antarctic Peninsula: New paleomagnetic pole from the James Ross Basin
title_fullStr Late Cretaceous paleogeography of the Antarctic Peninsula: New paleomagnetic pole from the James Ross Basin
title_full_unstemmed Late Cretaceous paleogeography of the Antarctic Peninsula: New paleomagnetic pole from the James Ross Basin
title_sort late cretaceous paleogeography of the antarctic peninsula: new paleomagnetic pole from the james ross basin
url http://hdl.handle.net/20.500.12110/paper_08959811_v91_n_p131_Milanese
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