\begin{table}%t5
  \caption{Results of our $\chi^2$-fit presented in Fig.~\ref{figure:fitting}. The used method is     described in Schegerer et~al.~(\cite{schegerer}) in detail. The underlying conti\-nuum is     estimated by a single blackbody function with the temperature $T$. ``RMC'' stands for 
    relative mass contribution, ``am.--sma.'' for amorphous, $0.1\ {\rm \mu m}$-small,     ``am.--la.'' for amorphous, $1.5\ {\rm \mu m}$-large and ``crys.'' for     crystalline silicate dust grains. 
    The crystalline component includes small and large silicate species: forsterite, enstatite, and     quartz.  See text for further discussion.}
  \label{table:fitting}
  %\centering
$$
  \begin{tabular}{lcccr}\hline\hline
     & Baseline length & Resolution & Silicate & RMC \\ \hline
     & & & am.--sma. & $(15 \pm 3)\%$ \\
     \raisebox{-1.5ex}[.5ex][.5ex]{A} &\raisebox{-1.5ex}[.5ex][.5ex]{single-dish}& 
     $70\ {\rm AU}$ & am.--la. & $(82 \pm 3)\%$ \\
     & & ($520\ {\rm mas}$) & crys. & $(3 \pm 1)\%$ \\
     & & & $T$ & $(450 \pm 3)\ {\rm K}$ \\ \hline
     & & & am.--sma & $(7 \pm 3)\%$ \\
     \raisebox{-1.5ex}[.5ex][.5ex]{B} & \raisebox{-1.5ex}[.5ex][.5ex]{$49\ {\rm m}$} & 
     $2.8\ {\rm AU}$ & am.--la. & $(82 \pm 5)\%$ \\
     & & ($21\ {\rm mas}$) & crys. & $(11 \pm 2)\%$ \\
     & & & $T$ & $(557 \pm 5)\ {\rm K}$ \\ \hline
     & & & am.--sma & $(1 \pm 1)\%$ \\
     \raisebox{-1.5ex}[.5ex][.5ex]{C} & \raisebox{-1.5ex}[.5ex][.5ex]{$78\ {\rm m}$} & 
     $1.8\ {\rm AU}$ & am.--la. & $(80 \pm 4)\%$ \\
     & & ($13\ {\rm mas}$) & crys. & $(19 \pm 2)\%$ \\
     & & & $T$ & $(722 \pm 9)\ {\rm K}$ \\  
    \hline
  \end{tabular}
  $$
\end{table}