The formation of nanometer twins of rutile and its textural characteristics in UHP eclogite.;

Deformation features of gneiss and UHP eclogite from ductile shear zone and its relation with seismic velocity anisotropy: Evidences from core samples at depth of 680 ~ 1200m of CCSD;

There still have been some disputable opinions on the UHP eclogites in western Dabieshan,especially regarding the stability of glaucophane-and kyanite-bearing assemblages in eclogites,their peak PT conditions and mineral assemblages,and the mineral evolution and fluid activity during early HP retrograde stage.

The understanding of deformation mechanism from ultrahigh pressure eclogite is crucial for the construction of geodynamic models of orogenic belt.

Based on field geological survey and mapping, and thorough research into regional eclogites and theirwall rocks,we name a suite of rock association together with eclogite subject to high-to ultra-hish-Pmetamorpism the eclogite belt and divide the wall rocks in to syngenetic,paragenetic and epigeneticones.