Palaeomagnetic dating and determination of tectonic tilting: A study of Mesozoic-Cenozoic igneous rocks in central West Portugal

Samples of igneous rocks (36 sites, 218 samples) associated with two main phases of the evolution of the Lusitanian Basin can be dated magnetically to latest Jurassic-early Cretaceous or late Cretaceous-Eocene. Directions of remanence in rocks belonging to the older phase require a 35° rotation to b...

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Autor principal: Pereira, J.L
Otros Autores: Rapalini, A., Tarling, D.H, Fonseca, J.
Formato: Capítulo de libro
Lenguaje:Inglés
Publicado: 1996
Acceso en línea:Registro en Scopus
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100 1 |a Pereira, J.L. 
245 1 0 |a Palaeomagnetic dating and determination of tectonic tilting: A study of Mesozoic-Cenozoic igneous rocks in central West Portugal 
260 |c 1996 
270 1 0 |m Pereira, J.L.; School of Environmental Sciences, University of East Anglia, Norwich NR4 7TJ, United Kingdom 
506 |2 openaire  |e Política editorial 
504 |a Aires-Barros, L., Actividade Magmea Pas-Palaeozsica no Continente Portugues - Elementos para una Sintese Critica (1979) Ciencias da Terra, 5, pp. 145-198 
504 |a Besse, J., Courtillot, V., Revised and synthetic Apparent Polar Wander Paths of the African, Eurasian, North American and Indian Plates and True Polar Wander since 200 Ma (1991) Journal of Geophysical Research, 96, pp. 4029-4050 
504 |a Fisher, R.A., Dispersion on a sphere (1953) Proceedings of the Royal Society of London, A217, pp. 295-305 
504 |a Fonseca, J., (1989) Seismicity and Regional Tectonics of the Estremadura, SW Portugal, , PhD Thesis, University of Durham, United Kingdom 
504 |a Freund, R., Tarling, D.H., Preliminary Mesozoic palaeomagnetic results from Israel and inferences for a microplate structure in the Lebanon (1979) Tectonophysics, 60, pp. 189-205 
504 |a Galdeano, A., Moreau, M.G., Pozzi, G.P., Berthou, P.Y., Malot, J.A., New Palaeomagnetic Results from Cretaceous sediments near Lisbon, Portugal and Implications for the Rotation of Iberia (1989) Earth and Planetary Science Letters, 92, pp. 95-106 
504 |a Guiry, F., (1984) Evolution Sedimentaire et Dynamique du Bassin Marginale Ouest-Portugais au Jurassique, Province d' Estremadure (Secteur de Caldas da Rainha-Montejunto), , Thèse d'État, Université de Lyon I, France 
504 |a Kirschvink, J.L., The least-squares line and plane and the analysis of palaeomagnetic data (1980) Geophysical Journal of the Royal Astronomical Society, 62, pp. 699-718 
504 |a Mcelhinny, M.W., (1973) Palaeomagnetism and Plate Tectonics, , Cambridge University Press 
504 |a Peirera, J.L.V., Fonseca, J.F.B.D., Rapalini, A., Tarling, D.H., Palaeomagnetic study of fault re-activation: A progress report (1992) 23rd General Assembly European Seismological Community, p. 16. , Prague 
504 |a Estudo Paleomagnetico da Reactivacao de Falhas (1992) 8th Conference Nacional Fisica, pp. 429-430. , Portugal 
504 |a Ribeiro, A., Antunes, M.T., Ferreira, M.P., Rocha, R.B., Soares, A.F., Zbyszeswki, G., (1980) Introduction la Geologie Generale du Portugal, , Serviços Geolôgicos de Portugal, Lisboa, Portugal 
504 |a Tarling, D.H., (1983) Palaeomagnetism, , Chapman & Hall, London 
504 |a Secular variations of the geomagnetic field - The archaeomagnetic record (1988) Secular Solar and Geomagnetic Variations in the Last 10 000 Years, pp. 349-365. , STEPHENSON, F. R. & WOLFENDALE, A. W. (eds) Kluwer Acad. Publ., Dordrecht 
504 |a Symons, D.T.A., A Stability Index of remanence in palaeomagnetism (1967) Geophysical Journal of the Royal Astronomical Society, 12, pp. 443-448 
504 |a Fonseca, J., Rapalini, A., Pereira, J.L., (1992) Investigative Palaeomagnetic Studies of Rocks in Southern Portugal, , Unpublished British Council report 
504 |a Van Der Voo, R., (1993) Palaeomagnetism of the Atlantic, Tethys and Iapetus Ocean, , Cambridge University Press 
504 |a Zijderveld, J.D.A., Renewed Palaeomagnetic Study of the Lisbon Volcanics and Implications for the Rotation of the Iberian Peninsula (1970) Journal of Geophysical Research, 76, pp. 3913-3921 
520 3 |a Samples of igneous rocks (36 sites, 218 samples) associated with two main phases of the evolution of the Lusitanian Basin can be dated magnetically to latest Jurassic-early Cretaceous or late Cretaceous-Eocene. Directions of remanence in rocks belonging to the older phase require a 35° rotation to become consistent with directions from stable Europe, while those of younger age do not require such rotation. On a finer scale, the remanent directions can be used to ascertain the probable tectonic tilt at different times of the igneous activity and hence provide intermediate evidence on the tectonic evolution of this area, including rotations of individual tectonic blocks about both vertical and horizontal axes.  |l eng 
593 |a Department of Geological Sciences, University of Plymouth, Plymouth PL4 8AA, United Kingdom 
593 |a School of Environmental Sciences, University of East Anglia, Norwich NR4 7TJ, United Kingdom 
593 |a Departamento de Ciencias Geologicas, Fac. de Cencos Exactas y Naturales, Ciudad Universitaria, 1428 Buenos Aires, Argentina 
593 |a Departamento de Fisica, Instituto Superior Ticnico, 1096 Lisboa, Portugal 
700 1 |a Rapalini, A. 
700 1 |a Tarling, D.H. 
700 1 |a Fonseca, J. 
773 0 |d 1996  |g v. 105  |h pp. 111-117  |p Geol. Soc. Spec. Publ.  |x 03058719  |t Geological Society Special Publication 
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