New paleomagnetic results from Neogene sedimentary sequences from the Belie chain (Spain) are here presented. Sedimentary basins located in different areas were selected in order to obtain paleornagnetic data from structural domains that experienced different tectonic evolution during the Neogene. Whereas no rotations have been evidenced in the Late Tortonian sediments in the Guadalquivir foreland basin, clockwise vertical axis rotations have been measured in sedimentary basins located in the central part of the Belies: the Aquitanian to Messinian sediments in the Alcala la Real basin and the Tortonian and Messinian sediments in the Granada basin. Moreover, counterclockwise vertical axis rotations, associated to left lateral strike-slip faults have been locally measured from sedimetary basins in the eastern Belies: the Middle Miocene to Lower Pliocene sites from the Lorca and Vera basins and, locally, the Tortonian units of the Huercal-Overa basin. Our results show that, conversely from what was believed up to now, paleomagnetic rotations continued in the Belies after Late Miocene, enhancing the role of vertical axis rotations in the recent tectonic evolution of the Gibraltar Arc. (c) 2006 Elsevier B.V. All rights reserved.
Mattei, M., Cifelli, F., Rojas, I.m., Blanc, A.c., Comas, M., Faccenna, C., et al. (2006). Neogene tectonic evolution of the Gibraltar Arc: New paleomagnetic constrains from the Betic chain. EARTH AND PLANETARY SCIENCE LETTERS, 250(3-4), 522-540 [10.1016/j.epsl.2006.08.012].
Neogene tectonic evolution of the Gibraltar Arc: New paleomagnetic constrains from the Betic chain
MATTEI, Massimo;CIFELLI, FRANCESCA;FACCENNA, CLAUDIO;
2006-01-01
Abstract
New paleomagnetic results from Neogene sedimentary sequences from the Belie chain (Spain) are here presented. Sedimentary basins located in different areas were selected in order to obtain paleornagnetic data from structural domains that experienced different tectonic evolution during the Neogene. Whereas no rotations have been evidenced in the Late Tortonian sediments in the Guadalquivir foreland basin, clockwise vertical axis rotations have been measured in sedimentary basins located in the central part of the Belies: the Aquitanian to Messinian sediments in the Alcala la Real basin and the Tortonian and Messinian sediments in the Granada basin. Moreover, counterclockwise vertical axis rotations, associated to left lateral strike-slip faults have been locally measured from sedimetary basins in the eastern Belies: the Middle Miocene to Lower Pliocene sites from the Lorca and Vera basins and, locally, the Tortonian units of the Huercal-Overa basin. Our results show that, conversely from what was believed up to now, paleomagnetic rotations continued in the Belies after Late Miocene, enhancing the role of vertical axis rotations in the recent tectonic evolution of the Gibraltar Arc. (c) 2006 Elsevier B.V. All rights reserved.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
