| Institution: | (1)Institute of Geology, Chinaese Academy of Geosciences, Beijing 100037 ,China;
(2)China University of Geosciences, Wuhan 430074 ,China;
(3)National University of Australia, G.P.O. Box 4, Canberra, A.C.T. 2601, Australia ,China |
| Abstract: | This note reports the SHRIMP U-Pb data of zircons from the Caledonian Xiongdian eclogite, western Dabie Mountains. Zircons from the rock occur mainly in garnet and other metamorphic minerals with sharp boundaries and exhibit textures growing under metamorphic conditions. Analyses of 7 grains give 206Pb/238U ages ranging from 335 to 424 Ma, showing a certain degree of radiogenic lead loss. This suggests a minimum age of (424±5) Ma for the metamorphic zircons, as well as the high-pressure metamorphic event. The outer peripheral zone of a zircon gives 206Pb/238U age of about 300 Ma. Combined with Sm-Nd, 40Ar-39Ar, U-Pb and 207Pb/206Pb ages, the peak metamorphism of the Xiongdian eclogite is documented between 424—480 Ma. |
