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Zircon (ZrSiO4) from Naegi and Ohro granitic pegmatites, Japan and from Saigon alkali basalt, Vietnam. were mineralogically characterized by inductively couples plasma mass spectrometry (ICP-MS), electron-microprobe analysis (EMPA), X-ray powder diffraction, micro-Raman spectroscopy and leaching experiment. The powder XRD and Raman spectra analyses show that the degree of metamictization increases in the following order: Saigon (crystalline), Ohro (partly metamict) and Naegi zircons (fully metamict). Quantitative analytical results by the EMPA indicate that the Naegi and Ohro zircon samples contain a large amount of REE2O3, while REE2O3 contents in Saigon zircon are below detection limit. The leaching experiments using a solvent 1 for the present zircons under the condition at a room temperature to 250 degrees C and retention time of 30 h resulted in about 100%, 50% and 1% recoveries of REE from the Naegi, Ohro and Saigon zircons, respectively. Leaching experiments for the Naegi zircon at different temperatures and retention time 30 h, showed that a significant amount of REE was leached out at the temperature above 150 degrees C, although REE were hard to be leached at a room temperature (about 25 degrees C). Therefore, both low crystallinity of zircon and higher leaching temperature are requisite for effective leaching of REE from zircon. (C) 2011 Elsevier B.V. All rights reserved.