The　rheological　characters　of　omphacites　in　Dabie　ultra-high-pressure　eclogite　have　been　studied　in　terms　of　fabric,　dislocation　and　micro-structures.　1.　The　eclogite　has　undergone　high-temperature　deformation,　thus　forming　omphacite　lattice　preferred　orientation.　In　addition　to　creep　dislocation,　the　omphacite　ductile　deformation　may　have　other　mechanisms,　such　as　diffusion　creep　and　grain　boundary　migration.　2.　The　main-phase　deformation　of　eclogite　is　coaxial,　but　asymmetry　strain　also　exists　due　to　strain　partitioning　in　the　Dabie　orogenic　belt.　3.　The　twin　measured　by　the　universal　stage　is　(100),　indicating　that　omphacite　high-T　deformation　was　superimposed　by　low-T　deformation.　4.　Subgrain　structure　is　common　in　omphacite,　but　the　deformation　features　of　the　omphacites　in　the　Shuanghe　area　and　Bixiling　area　are　different,　the　latter　being　dominated　by　dynamic　recrystallization.　5.　The　Flinn　plots　show　that　the　strain　of　omphacite　belongs　to　the　constriction　ellipsoid　and　stretching　strain,　which　is　similar　to　the　result　of　the　omphacite　fabric　analysis.