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对利用氖同位素体系标定地幔柱的新方法进行评述,介绍 Matsumoto 等在澳大利亚用磷灰石中地幔派生矿物的流体包裹体氖同位素组成研究地幔柱的方法原理及成果,并指出该方法的不足之处。这对于促进有关地幔柱的地球化学示踪剂的研究很有指导意义。
This paper reviews the new method of calibration of mantle plumes by neon isotope system and introduces the principle and results of mantle plume research by using the neon isotope composition of fluid inclusions derived from the mantle-derived minerals of apatite in Australia by Matsumoto et al. Department. This is very instructive for the study of geochemical tracer for mantle plumes.