style="MARGIN: 0cm 0cm 0pt" class=MsoNormal>///Beryl occurred in mineral association of granite greisened muscovite, albite, beryl and quartz. Goniometry indicated that the single form crystal face growth is in turn c{0001}, s{112-1}, p{101-1}, m{101-0} and v{213-1}, the next place is n{459-4} and a{112-0}. The fluid inclusion temperatures tested by homogenous method and ingredient analysis by laser Raman spectroscope(LRS) all revealed that the tabular beryl has grown in medium-high temperature(about space prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:chmetcnv w:st="on" UnitName="℃" SourceValue="303" HasSpace="True" Negative="False" NumberType="1" TCSC="0">303 style="FONT-FAMILY: 宋体; mso-bidi-font-family: 宋体" lang=EN-US>℃st1:chmetcnv>)and stabling thermodynamics, the gas and the liquid inclusion mainly composed by H2O, CO2 and micro CH4, N2. CO2 and micro CH4, N2 possible concerns to the carbonate wallrock.