style="MARGIN: 0cm 0cm 0pt" class=MsoNormal>The gneissose granites developed very much neighboring kawabulake area in the espace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:place w:st="on"><st1:PlaceName w:st="on">asternst1:PlaceName> <st1:PlaceName w:st="on">Tianshanst1:PlaceName> <st1:PlaceType w:st="on">Mountainsst1:PlaceType>st1:place>. According to the fielded characteristics, these granites can be divided into two types, namely bearing-porphyritic and non-bearing-porphyritic gneissose granites, their gneissosities formed due to reconstruction of ductile shearing. The fielded investigations showed that gneissose granites intruded into obviously Xingxingxia Group and/or Kawabulake Group, and were intruded into by the carboniferous granites. At the same time, the Upper Devonian strata had hardly ductile deformations in the west of the study area. So that, the time of the ductile shearing deformation can be limited between Mid-Silurian to before Dvonian period.