Petrologic geochemistry and isotopic chronology of the eclogites suggest that most of the eclogites in northern Dabie Mountains produced from the Triassic Yangtze subducted continental crust (lower crust and formed during the deep subduction) and the metamorphosed mafic-untramafic belt with eclogite, marble and meta-peridotite blocks around the Mozitan-Xiaotian fault zone may represent the meta-tectonic melange produced during the active subduction of an ancient oceanic slab and subsequent collision between the Yangtze and North China continental plates. The cooling history of the eclogites from ～900 ℃ to 300 ℃ can be subdivided into three stages: one isothermal stage and two rapid cooling stages. The initial stage between (230±6) and 210 Ma was a near-isothermal or temperature rise process corresponding to the retrograded metamorphism of granulite-facies with a rapid uplift of 4 nun/a, then two fast cooling stages occurred with cooling rate of ～10 ℃/Ma during 210 Ma to (172±3) Ma and ～4 ℃/Ma during (172±3) Ma to 130 Ma. After the peak metamorphism of eclogite-facies, their initial isothermal stage with slower uplift rate and cooling rate and high-T overprinting of granulite-facies metamorphism is the major difference between the eciogites in northern Dabie Mountains from those in southern Dabie Mountains. This may be one of the most important reasons to preserve few evidences of earlier ultrahigh-pressure metamorphism.