• Aucun résultat trouvé

Active faulting at the western tip of the Gulf of Corinth, Greece, from high-resolution seismic data

N/A
N/A
Protected

Academic year: 2021

Partager "Active faulting at the western tip of the Gulf of Corinth, Greece, from high-resolution seismic data"

Copied!
15
0
0

Texte intégral

Loading

Figure

Fig. 2 displays the morphological units of the sea fl oor relief interpreted in this study
Fig. 4.Proposed correlation between the chronostratigraphy developed by Bell et al. (2008)and our data set
Fig. 6. Map of offshore faults identified in this study. Onshore faults from Ford et al
Fig. 7. S-N Sparker seismic profile in the Nafpaktos Basin. See Fig. 2 for its location
+6

Références

Documents relatifs

En fonction de l’endroit de pénétration (fourchette, lacunes de la fourchette, glomes de la fourchette, partie crâniale de la sole) et de la direction (hori- zontale,

L’archive ouverte pluridisciplinaire HAL, est destinée au dépôt et à la diffusion de documents scientifiques de niveau recherche, publiés ou non, émanant des

- .ايرصب قاعملا ىدل تاذلا موهفم و يسفنلا نملأا نيب ةيرهوج قورف دجوت ( نم ةنيع ثحابلا لمعتسا تايضرفلا قيقحت دصق 22 نم ةبلاطو ابلاط) نيفوفكملا ةبلطلا

Model simulations indicate that polar surface waters will become undersaturated for aragonite in the near future for the Arctic (atmospheric carbon dioxide of 400–450 ppm) and

Single crystal growth, crystal structure and surface characterisation of the binary phase Al45Cr7.. Pascal Boulet, Marie-Cécile de Weerd, Emilie Gaudry, Julian Ledieu,

Furthermore, as for MTTs with collinear magnetic configurations, we report the magnetocurrent as a function of the magnetic layer thickness that increases with layer thickness up

For m = 0.2 (non-linear case, see figure 2), more discrepancies occur between the different approximations and the FFT method especially at large physical times when the

Authors Relation Roughness measuremet principle SSD measuring principle Sample Preparation method considered Material used to establish the relation Hed [13] SSD