University of Aveiro : Depart. of Geosciences : Teachers : Fernando Rocha : Publications

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Published articles

Clay mineralogy used for the definition of paleosurfaces in the Tertiary and Quaternary of the Aveiro sedimentary basin. Mémoires des Sciences de la Terre, Ecole des Mines de Paris, Vol. 18, 1991, pp. 31-38 (F. Rocha & C. Gomes).

Fibrous clay minerals as morpho-climatic markers in the Aveiro sedimentary basin. Min. et Petr. Acta, Vol. XXXV-A, 1992, pp. 217-226 (F. Rocha & C. Gomes).

Evolution of the Aveiro lagoon during the last 500 years based on clay mineralogy. Min. et Petr. Acta, Vol. XXXV-A, 1992, pp. 105-110 (H. Delgado, F. Rocha & C. Gomes).

Discrimination of Tertiary and Quaternary; lithostratigraphical units in the Aveiro region on the basis of clay minerals. Acta Universitatis Carolinae Geologica. (Praga), 38, pp. 381-390, 1994 (F. Rocha & C. Gomes).

Clay mineralogy used for the definition of climatic oscillations during the Quaternary in the Aveiro lagoon (Portugal) Acta Universitatis Carolinae Geologica. (Praga), 38, pp. 153-161, 1994 (H. Delgado, F. Rocha & C. Gomes).

Paleoenvironmental reconstruction of the Aveiro region during Cretaceous based on clay mineralogy. Cretaceous Research, 16, 1995, pp. 187-194 (F. Rocha & C. Gomes).

Mineralogical characterization of the fine fraction of the beach and dune sediments situated between Espinho and Torreira (Portugal) - a geostatistical approach. Cuaternario y Geomorfologia, 12(3/4), 1998, pp. 49-56 (J. Vidinha, F. Rocha, C. Andrade & C. Gomes).

Statistical analysis of mineralogical parameters used as lithostratigraphic markers. Application to Quaternary sediments of the littoral between Espinho and Furadouro (Portugal).Boletin Instituto Español de Oceanografia, 15(1-4), 1999, pp. 303-312 (A. Machado, F. Rocha & C. Gomes).

Geostatistical analysis of the influence of textural, mineralogical and geochemical parameters on the geotechnical behaviour of the “Argilas de Aveiro” formation (Portugal). Clay Minerals, 34, 1999, pp. 109-116 (C. Galhano, F. Rocha & C. Gomes).

Characterization and datation of Holocene mud layers from the urban area of Aveiro (Portugal). Cuaternario y Geomorfologia, 13(1/2), 1999, pp. 45-52 (F. Rocha, A.C. Galhano & C. Gomes).Statistical analysis of mineralogical parameters used as lithostratigraphical markers. Acta Universitatis Carolinae Geologica (Praga), 45(2-4), pp. 147-151, 2000 (F. Rocha, J. Vidinha, P.S. Caetano & C. Gomes).

Mineralogy of the fine fraction of the sediments as dynamic sedimentary tracers - NW Iberian Margin. Thalassas, 17, 2001, pp. 35-44 (A. Oliveira, F. Rocha, A. Rodrigues & J.A. Dias).

First data on mineralogy and geochemistry of Tunisian Palaeozoic clays. Boletin Soc. Española de Mineralogia, 24, 2001, pp. 59-67 (F. Jamoussi, A. Lopez Galindo, S. Karbachi, F. Rocha, C. Gomes, J. Duplay, R. Alouani & F. Zargouni).

Mineralogical characterisation of stream sediments from Portugal. Boletin Soc. Española de Mineralogia, 24, 2001, pp. 69-80 (F. Rocha, A. Ferreira & M.S. Pinto).

Palaeozoic clays of Tunisia. Geologica Carpathica, 53(2), 2002, pp. 1-6 (F. Jamoussi, S. Karbachi, F. Rocha, A. Lopez Galindo, C. Gomes, J. Duplay, R. Alouani & F. Zargouni).

Clay minerals of the sedimentary cover from the Northwestern Iberian shelf. Progress in Oceanography, Elsevier, 52(2-4), 2002, pp. 233-247 (A. Oliveira, F. Rocha, A. Rodrigues, J. Jouanneau, J.A. Dias, O. Weber & C. Gomes). Environmental changes of the Santo André coastal area (SW Portugal) during the last 14 000 years: the sedimentological and geochemical records. Accepted for publication, The Holocene (M.C. Freitas, C. Andrade, F. Rocha, C. Tassinari, M. Munhá, A. Cruces & J. Vidinha).

Tectonostratigraphy of middle and upper Palaeozoic black shales from Porto–Tomar–Ferreira do Alentejo shear zone (W Portugal): new perspectives on the Iberian Terrane. Accepted for publication, GEOBIOS Journal, 2002. (H.I. Chaminé, L.C. Gama Pereira, P.E. Fonseca, L.P. Moço, J.P. Fernandes, F. Rocha, D. Flores, A. Pinto de Jesus, C. Gomes, A.A. Soares de Andrade & A. Araújo).

 

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