\overlays{1}{%
\begin{slide}{Domaines d'application}
\vskip 0.2cm
M\'ecanisme dynamo au sein du noyau terrestre.
\vskip 0.3cm
\centerline{
\epsfxsize 0.7\linewidth \epsffile{/home/narteau/HERBE/ECRIT/CNRS/proj1.eps}}
\vskip 0.1cm
\hfill {\LemonChiffon Narteau et al. (2000a)}
\end{slide}
}

\overlays{1}{%
\begin{slide}{Domaines d'application}
\vskip -0.3cm
\begin{minipage}{0.5\linewidth}
\centerline{Limites temporelles}
\centerline{de la loi d'Omori}
\vskip 3.5cm
{\hfill {\LemonChiffon Narteau et al. (2002a)}}
  \end{minipage}
  \begin{minipage}{0.5\linewidth}
        \centerline{
\epsfxsize \linewidth \epsffile{/home/narteau/ECRIT/MCONF/fififrench.eps}}
\centerline{ }
 \end{minipage}
\end{slide}
}

\overlays{1}{%
\begin{slide}{Domaines d'application}
\vskip -0.3cm
\begin{minipage}{0.5\linewidth}
\centerline{Thermodynamique des}
\centerline{populations de fractures}
\vskip 3.5cm
{\hfill {\LemonChiffon Narteau et al. (2002b)}}
  \end{minipage}
  \begin{minipage}{0.5\linewidth}
        \centerline{
\epsfxsize \linewidth \epsffile{/home/narteau/ECRIT/IRD/COMPLEX/figpap.eps}}
\centerline{ }
 \end{minipage}
\end{slide}
}


\overlays{1}{%
\begin{slide}{Domaines d'application}
\vskip 0.2cm
\begin{minipage}{0.5\linewidth}
\centerline{Rugosit\'e de petite}
\centerline{\'echelle \`a la}
\centerline{fronti\`ere noyau-manteau}
\vskip 3.5cm
{\hfill {\LemonChiffon Narteau et al. (2001)}}
  \end{minipage}
  \begin{minipage}{0.5\linewidth}
        \centerline{
\epsfxsize 0.9\linewidth \epsffile{/home/narteau/ECRIT/FIGURE/FIG3_zoom.eps}}
  \end{minipage}
\end{slide}
}

\overlays{1}{%
\begin{slide}{Domaines d'application}
\vskip -0.5cm
\begin{minipage}{0.5\linewidth}
\centerline{Sismicit\'e le long d'un}
\centerline{segment de faille}
\vskip 4cm
{\hfill {\LemonChiffon Narteau et al. (2000b)}}
  \end{minipage}
  \begin{minipage}{0.5\linewidth}
        \centerline{
\epsfxsize \linewidth \epsffile{/home/narteau/HERBE/ECRIT/CNRS/proj2.eps}}
\centerline{ }
 \end{minipage}
\end{slide}
}


