Advances and Perspectives of Experimental Geochemistry
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摘要: 实验地球化学主要通过高温高压实验模拟,对元素和同位素在地球内部条件下的行为、性质和效应进行研究,从而对成岩成矿、岩浆演化、流体交代、壳−幔−核分异等地质现象和过程进行制约. 实验地球化学的最初诞生,主要是针对传统地球化学、岩石学和矿床学研究中遇到的难以解决问题进行正演辅助. 实验地球化学的发展,与高温高压实验设备和现代分析技术的成熟和完善密切相关. 近半个世纪以来,实验地球化学的不断成长壮大,极大促进了传统地球化学乃至整个地球科学相关领域的发展. 在未来的10到20年内,实验地球化学有望在以下3个方面进一步加强和取得重要科研成果:(1)深部地球和早期地球;(2)挥发分和地球宜居性;(3)行星形成演化实验模拟.Abstract: Experimental geochemistry involves the simulation of the physical and chemical conditions of the Earth's interior. By this, the behavior, nature and effects of elements and isotopes are studied experimentally, so as to constrain processes such as petrogenesis and mineralization, magma evolution, fluid metasomatism, and differentiation. The field of experimental geochemistry emerged as a tool to offer forward modeling for challenging issues that are difficult to address by studies with traditional geochemistry and petrology. The rapid development of the field is attributed to the improvement of facilities for generating high‐pressure and high‐temperature conditions and the availability of modern analytical techniques. In the past about half century, the growing research in the field of experimental geochemistry has greatly promoted the development of traditional geochemistry and even the entire earth science related fields. In the next one or two decades, experimental geochemistry is expected to further strengthen important scientific achievements in the following aspects: (1) deep Earth and early Earth; (2) volatiles and habitability of the Earth; (3) experimental simulations and planetary science.
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图 2 行星起源、挥发分和地球演化
修改自Gaillard and Scaillet(2004)
Fig. 2. Planetary origin, volatiles and Earth's evolution
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