本文为中国核工业地质局“十一五”基础科研项目 (编号 YK08), 内生金属矿床成矿机制研究国家重点实验室研究项目(编号2008 I 04)的成果。
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.2013. Doubts about “the Closure Temperature of U Pb Isotopic Systerm in the Zircon Crystallized from Granitic Magma ≥ 850℃”: Evidences of Element Diffusion Theory and Comparision between the Zircon U Pb Ages and the Whole rock Rb Sr Ages of Granite Plutons[J]. Geological Review,59(1):63-70.