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锆石在探究岩浆形成与演化中的应用
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Abstract:
锆石作为一种稳定的副矿物，在地球上各种岩浆岩、变质岩与沉积岩中均有出现。由于其耐高温和抗腐蚀，富含U等元素，并且具有较高的封闭温度，锆石一直是U-Pb同位素测年的理想矿物。近年来随着原位微区测试技术的发展，对锆石的应用研究已经从传统的U-Pb同位素测年逐渐转向微区同位素和微量元素示踪领域。本文主要是在收集与整理国内外相关研究成果的基础上，系统地归纳总结锆石在确定岩浆结晶年龄、识别岩浆源区组成、反演岩浆物理化学条件、识别岩浆结晶分异过程和判别岩浆形成的板块构造环境等方面的应用，为未来运用锆石深入探究岩浆形成与演化过程提供重要参考。
As a stable submineral, zircon occurs in all kinds of magmatic rocks, metamorphic rocks and sedimentary rocks on Earth. Due to its high temperature and corrosion resistance, high concentration of elements such as U, and high sealing temperature, zircon has been an ideal mineral for U-Pb isotope dating. In recent years, with the development of in situ microzone measurement technology, the applied research of zircon has gradually shifted from the traditional U-Pb isotope dating to the field of microzone isotope and trace element tracing. Based on the collection and collation of relevant research results at home and abroad, this paper systematically summarizes the application of zircon in determining the crystallization age of magma, identifying the composition of magma source region, inverting the physical and chemical conditions of magma, identifying the crystallization differentiation process of magma, and discriminating the plate tectonic environment of magma formation. It provides important reference for further study of magma formation and evolution by zircon in the future.
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