File:Plate tectonic W-Méditerranée (2).jpg

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Français : Situation des plaques tectoniques W-Méditerranée au Jurassique sup. (d'après Rosenbaum et al. (2002) servant de cadre général aux cartes paléogéographiques, montrant l'évolution de la marge N-briançonnaise (et de la plateforme carbonatée associée) dans les Préalpes médianes au Dogger. Cette portion de la microplaque briançonnaise se situait, au Jurassique, à peu près au niveau de Monaco ( à droite de Br sur la figure).
English: W - Mediterranean plate tectonic (Rosenbaum et al., 2002) during late Jurassic times. Paleogeographic maps and briançonnais margin evolution in the Prealps (Dogger carbonate platform) is shown in following fig. This portion of the Briançonnais microplate was situated roughly in front of Monaco (Br on fig.) or eastward, during the Jurassic.
Date
Source Tectonophysics, 339; 117-126.
Author Rosenbaum et al (2002).

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current09:06, 12 October 2011Thumbnail for version as of 09:06, 12 October 2011901 × 768 (97 KB)Septfontaine (talk | contribs)

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