摘要
///Detailed structural analysis and mapping at a scale of 1∶10 000 at more than 30 key locations in combination with extensive regional field observations of UHP/HP metamorphic rocks in the Dabie-Sulu region, eastern China were carried out in order to reveal their structural geometry, deformation conditions and rheological evolution. Preliminary results show that the wellexposed relict UHP/HP eclogitefacies rocks, outlining a giant UHP/HP metamorphic belt in eastern China, provide a window into Triassic continental subduction/collision-belt processes between the Yangtze craton in the south and the Sino-Korean craton in the north. The observed microstructures and fabrics clearly indicate that the deformation mechanism operating in the rocks, within the UHP/HP metamorphic belt, was dominated by plastic flow during both the UHP/HP eclogite and posteclogitefacies deformation histories.