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Ca同位素地球化学及其地质应用

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Ca作为主要的造岩元素,在各类地质过程均能显示出不同程度的分馏,使之成为研究不同地质过程的潜在地球化学指标和示踪剂。随着分析技术的发展,作为新兴的Ca同位素被越来越多地应用于地质学的不同领域,尤其在近十年取得了丰富的研究成果。在简要介绍Ca同位素标准物质和分析方法的基础上,详细阐述了Ca同位素在地质学 3 个领域方面的应用,包括:1)Ca同位素在行星地质方面的应用,探究陨石、月球等天体成因与演化过程以及早期地球特征;2)Ca同位素在深部地质过程方面的应用,可有效示踪地幔交代、大陆俯冲和深部碳循环等;3)Ca同位素在低温过程方面的应用,重建海水演化和河流、地下水与冷泉系统。通过上述重要地质过程中研究成果的系统总结,旨在加深对Ca同位素体系的深入理解,并对Mg-K-Ca多元同位素联合示踪的应用进行了展望。
Ca Isotope Geochemistry and Its Geological Applications
As the main rock-forming element,Ca can show different degrees of fractionation in vari-ous geological processes,making it a potential geochemical index and tracer for studying diverse ge-ological processes.With the development of analytical techniques,Ca isotope can be more precisely determined and has been more and more applied to different fields of geology.During the past dec-ade,lots of research results had been accumulated.Based on the brief introduction of Ca isotope ref-erence materials and analytical methods,this study elaborates the application of Ca isotope in three fields of geology,including:1)the application of Ca isotope in planetary geology,which aims to ex-plore the causes and evolution processes of the meteorites,moon and other celestial bodies,as well as the characteristics of the early Earth.2)the application of Ca isotope in tracing deep geological processes;these processes include mantle metasomatism,continental subduction and deep carbon cycle.3)the application of Ca isotope in low-temperature processes;these include reconstruction of seawater evolution and river,groundwater and cold spring systems.Through reviewing recent ad-vances in the above important geological processes,we tend to deepen the understanding of the Ca i-sotope system.In the end,the emerging application of Mg-K-Ca multi-isotope combined tracing is also prospected.

Ca isotopeplanetary geologydeep geological processlow-temperature processcom-bined application of multi-isotope

王慧丽、曹俊

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东华理工大学地球科学学院,330013,南昌

Ca同位素 行星地质 深部地质过程 低温过程 多元联合示踪

江西省自然科学基金面上项目

20232BAB203067

2024

江西科学
江西省科学院

江西科学

影响因子:0.286
ISSN:1001-3679
年,卷(期):2024.42(2)
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