Table of Contents
| Recent processes on Iberian Continental Shelf | |
| Ana Bernabeu, Federico Vilas | 173 |
| Preface | |
| A. Bernabeu, F. Vilas | 175-176 |
| The recorded evidence of AD 1755 Atlantic tsunami on the Gibraltar coast | |
| J. Rodríguez-Vidal, L. M. Cáceres, M. Abad, F. Ruiz, M. L. González-Regalado, C. Finlayson, G. Finlayson, D. Fa, J. M. Rodríguez-Llanes, G. Bailey | 177-193 |
| Spatial variability of surficial sediments on the northern shelf of the Alboran Sea: the effects of hydrodynamic forcing and supply of sediment by rivers | |
| P. Bárcenas, F. J. Lobo, J. Macías, L. M. Fernández-Salas, V. Díaz del Río | 195-214 |
| Erosion and accretion in the Ria de Aveiro inlet (N Portugal) and exportation of fine–grained sediments to the shelf | |
| V. Martins, C. Grangeia, C. C. Jesus, P. Martins, L. M. Laut, C. Sequeira, J.M. Dias, P. A. Silva, I. Abrantes, E. Ferreira da Silva, F. Rocha | 215-230 |
| The response of benthic foraminifera to pollution and environmental stress in Ria de Aveiro (N Portugal) | |
| V. Martins, C. Yamashita, S.H.M. Sousa, P. Martins, L.L.M. Laut, R.C.L. Figueira, M.M. Mahiques, E. Ferreira da Silva, F. Rocha, J.M. Alveirinho Dias | 231-243 |
Articles
| Geometry, structures and evolution of the western termination of the Alpine-Pyrenean Orogen reliefs (NW Iberian Peninsula) | |
| F. Martín González, N. Heredia | 103-120 |
| Variscan and Alpine structure of the hills of Barcelona: geology in an urban area | |
| P. P. Santanach, J. M. Casas, O. Gratacós, F. Sàbat, M. Liesa, J. A. Muñoz, F. Sàbat | 121-136 |
| Biostratigraphy and paleobiogeographic affinities of the Jurassic brachiopod assemblages from Sierra Espuña (Maláguide Complex, Internal Betic Zones, Spain) | |
| J.F. Baeza-Carratalá, F. García Joral, J.E. Tent-Manclús | 137-151 |
| New rodent faunas from Middle Miocene and Mio- Pliocene in the Cabriel Basin (Valencia, Spain) | |
| F.J. Ruiz-Sánchez, C. Santisteban, V.D. Crespo-Roures, M. Freudenthal | 161-172 |
Journal of Iberian Geology
ISSN 1698-6180
ISSN-e 1886-7995
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