Please use this identifier to cite or link to this item: http://hdl.handle.net/10174/17154

Title: Staircases of wave-cut platforms in western central Portugal (Cape Mondego to Cape Espichel) – relevance as indicators of crustal uplift Escadarias de terraços marinhos em Portugal centro-ocidental (Cabo Mondego ao Cabo Espichel) – relevância como indicadores de soerguimento crustal
Authors: Cunha, Pedro
Martins, António
Cabral, João
Gouveia, M.P
Buylaert, Jan-Pieter
Murray, Andrew
Editors: Díaz del Río, V.
Bárcenas, V.
L.M.Fernández-Salas, L.M.
López-González, N.
Palomino, D.
Rueda, J.L.
Sánchez-Guillamón, O.
Vázquez, J.T.
Keywords: marine/coastal terrace
wave-cut platform,
high sea-level
uplift
central Portugal
Issue Date: 21-Sep-2015
Publisher: V. Díaz del Río, P. Bárcenas, L.M. Fernández-Salas, N. López-González, D. Palomino, J.L. Rueda, O. Sánchez-Guillamón, J.T. Vázquez, Grupo de Geociencias Marinas (GEMAR) Centro Oceanográfico de Málaga; Instituto Español de Oceanografía; Ministerio de Economía y Competitividad
Citation: Cunha, P., Martins, A.,Cabral, J., Gouveia, M.P.,Buylaert, J.P., Murray, A. 2015. Staircases of wave-cut platforms in western central Portugal (Cape Mondego to Cape Espichel) – relevance as indicators of crustal uplift Escadarias de terraços marinhos em Portugal centro-ocidental (Cabo Mondego ao Cabo Espichel) – relevância como indicadores de soerguimento crustal.Resúmenes sobre el VIII Simposio EL MARGEN IBÉRICO ATLÁNTICO (MIA15), Málaga.p.137 -144
Abstract: This study addresses coastal terrace staircases of western central Portugal (Cape Mondego to Cape Espichel). Below the culminant marine unit, that records the last episode of aggradation before the ongoing stage of incision, several terrace levels are identified. The following methodology was used: a) production of geomorphological maps, combining analysis of detailed MDT’s and aerial photos, with field surveys calibrated with GPS data; b) stratigraphic and sedimentological study of the sedimentary deposits associated with the marine platforms; c) luminescence dating. On each terrace staircase, the number of platforms and their elevations are different, indicating differential uplift. Quartz OSL provided age estimates up ca. 150 kyr and post-IR IRSL on K-feldspar up to ca. 700 kyr for the marine terraces under study. Using the culminant platform as reference and assuming that it is 3.6 Ma old, uplift rates were estimated as ranging from 0.071 m/ky to 0.019 m/ky. The ongoing luminescence dating will provide the uplift rates estimated for the lower and middle marine terraces
URI: http://hdl.handle.net/10174/17154
Type: article
Appears in Collections:CGE - Artigos em Livros de Actas/Proceedings

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