{\rtf1 \ansi 
{\colortbl;
\red0\green0\blue0;
\red255\green255\blue255;
\red255\green0\blue0;
\red0\green255\blue0;
\red0\green0\blue255;
\red0\green255\blue255;
\red255\green0\blue255;
\red255\green255\blue0;
\red0\green0\blue128;
\red0\green128\blue128;
\red0\green128\blue0;
\red128\green0\blue128;
\red128\green0\blue0;
\red128\green128\blue0;
\red128\green128\blue128;
\red192\green192\blue192;
}
{\fonttbl {
\f0 Arial;}{
\f1 Symbol;}{
\f2 Times New Roman;}{
\f3 sans-serif;}{
\f4 Helvetica;}
}
{\*\generator Apache XML Graphics RTF Library;}
\fet0 \ftnbj \paperw11905 \paperh16837 \margt2948 \margb1814 \margl850 \margr850 \headery1133 \footery1814 \itap0 
\sectd {\header 
{\ri0 \chcbpat1 \li0 
{\b0 \cf1 \f3 \ri0 \i0 \ql \fs24 \li0 
}
}
{\b0 \cf1 \f3 \ri0 \i0 \ql \fs24 \li0 
{\ri0 \li0 
{\b0 \cf1 \f3 \ri0 \i0 \ql \fs24 \li0 
}
}
}}{\footer 
{\ri0 \li0 
{\b0 \cf1 \f4 \i0 \brdrt \brdrcf15 \brdrw20 \brdrdot \fs16 \brdrr \brdrcf15 \brdrw20 \brdrdot \brdrl \brdrcf15 \brdrw20 \brdrdot \ri0 \ql \li0 \brdrb \brdrcf15 \brdrw20 \brdrdot 
{\b0 \cf1 \f4 \ul0 \strike0 \i0 \fs16 \sa0 \sb0 
See Alexandrite Tsarstone collectors guide, Definition of Heavy minerals, 
}
{\field {\*\fldinst HYPERLINK "http://www.alexandrite.net/viewpage.html?id=GG-093-00003" }{\fldrslt 
{\b0 \cf5 \f4 \ul1 \strike0 \i0 \fs16 \sa0 \sb0 
http://www.alexandrite.net/viewpage.html?id=GG-093-00003
}}}
{\b0 \cf1 \f4 \ul0 \strike0 \i0 \fs16 \sa0 \sb0 
 (Minerals having a high specific gravity, which are separated in the laboratory from light minerals by use of heavy liquid, such as bromoform. Generally grains heavier than bromoform constitute the heavy minerals.) (as of ).
\par 
}
}
{\b0 \cf1 \f3 \ri0 \i0 \ql \fs24 \li0 
\tqr \tx11872 {\pard \cf1 \f3 \expnd-2 \tab }
\par 
}
{\b0 \cf1 \f3 \ri0 \i0 \ql \fs24 \li0 
\tqr \tx11872 {\pard \cf1 \f3 \expnd-2 \tab }
\par 
}
{\b0 \qc \cf1 \f4 \ri0 \i0 \fs20 \li0 
{\b0 \cf1 \f4 \ul0 \strike0 \i0 \fs20 \sa0 \sb0 
Page 
}
{\b0 \i0 \ul0 \fs20 \f4 \chpgn }
{\b0 \cf1 \f4 \ul0 \strike0 \i0 \fs20 \sa283 \sb0 
 of 
}
{\field {\*\fldinst { PAGEREF "end-seq" } }{\fldrslt# }}
\par 
}
}}
{\b0 \cf1 \f0 \ri0 \i0 \ql \fs24 \li0 
{\b0 \cf1 \f0 \ul0 \strike0 \i0 \fs24 
}
{\b1 \cf1 \f0 \ri0 \i0 \ql \fs32 \li0 
{\b1 \cf1 \f0 \ul0 \strike0 \i0 \fs32 \sa113 \sb0 
Heavy minerals
\par 
}
}
{\b0 \cf1 \f0 \ul0 \strike0 \i0 \fs24 
}
{\b0 \cf1 \f0 \ri0 \i0 \ql \fs24 \li283 
{\b0 \cf1 \f0 \ul0 \strike0 \i0 \fs24 
}
{\b0 \cf1 \f0 \ri0 \i0 \ql \fs24 \li283 
{\b0 \cf1 \f0 \ul0 \strike0 \i0 \fs24 \sa113 \sb226 
Heavy minerals
\par 
}
}
{\b0 \cf1 \f0 \ul0 \strike0 \i0 \fs24 
}
{\b0 \cf1 \f0 \ri0 \i0 \ql \fs24 \li283 
{\b0 \cf1 \f0 \ul0 \strike0 \i0 \fs24 \sa113 \sb0 
Minerals having a high specific gravity, which are separated in the laboratory from light minerals by use of heavy liquid, such as bromoform. Generally grains heavier than bromoform constitute the heavy minerals.
\par 
}
}
{\b0 \cf1 \f0 \ul0 \strike0 \i0 \fs24 
}
}
{\b0 \cf1 \f0 \ul0 \strike0 \i0 \fs24 
}
}
{\b0 \cf1 \f3 \ri0 \i0 \ql \fs24 \li0 
{\*\bkmkstart end-seq}{\*\bkmkend end-seq}
}}