锌同位素地球化学及应用研究进展  

Zinc isotope geochemistry and its applications: A critical review

作　　者：马蕾 李丹丹[1] 吕逸文 王勋 王泽洲[1] 李孟伦 杨春 瞿瑗汝 舒梓坦 刘盛遨[1] MA Lei;LI Dandan;LV Yiwen;WANG Xun;WANG Zezhou;LI Menglun;YANG Chun;QU Yuanru;SHU Zitan;LIU Sheng’ao(State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Beijing 100083,China)

机构地区：[1]中国地质大学(北京)地质过程与矿产资源国家重点实验室,北京100083

出　　处：《地球化学》2022年第2期161-175,共15页Geochimica

基　　金：国家自然科学基金项目(41603010,41622303)资助。

摘　　要：随着化学纯化技术的提高及质谱仪的开发与应用,锌同位素已成为近年来非传统稳定同位素地球化学的一个研究热点,人们对锌同位素地球化学的认识随着研究的深入有了极大提高。本文对锌同位素地球化学进行了全面的综述,追踪了锌同位素在地学领域最新的研究进展。目前,锌同位素已被广泛应用在天体化学、环境地球化学、古海洋、古环境重建以及深部碳循环等诸多地球科学及环境科学研究领域,展现出巨大的应用潜力。各领域的研究成果为推进锌同位素地球化学的发展做出了巨大贡献。The recent development of chemical purification and the application of multi-collector inductively coupled plasma mass spectrometry(MC-ICP-MS) has significantly improved the precision of Zn isotopic analysis.The studies of Zn isotopes have become a hot topic in the research field of non-traditional stable isotopes. At the same time, our knowledge of understanding the Zn isotope geochemistry has been greatly improved. This paper presents a comprehensive review of the latest research on Zn isotope geochemistry and updates its applications in Earth sciences. Zinc isotopes have been widely applied in many subjects, such as cosmochemistry, environmental geochemistry, paleoceanography, paleoenvironmental reconstruction, and the deep carbon cycle. These applications manifest the great potential of Zn isotopes in Earth and planetary sciences and contributes to the development of Zn isotope geochemistry.

关 键 词：锌同位素 分析方法 储库 分馏理论 地质及环境应用 

分 类 号：P597.2[天文地球—地球化学]