湖相碳酸盐碳、氧同位素与团簇同位素的研究进展

总结近年来传统碳、氧同位素及新兴团簇同位素在湖相碳酸盐中的研究进展,梳理湖相环境中碳酸盐同位素组成变化的影响因素及两种同位素方法在地质研究中的应用,探讨当前研究中存在的问题.湖相碳酸盐氧同位素组成受温度的影响较小,主要与湖盆水体的蒸发量和大气降水量有关,碳同位素组成则受湖水蒸发咸化作用以及湖泊有机质与无机质相互作用的共同控制;团簇同位素仅受温度单一因素的影响,是良好的碳酸盐温度计.指出湖相碳酸盐碳、氧同位素研究的两大方向:一是解决团簇同位素理论研究中存在的问题,尤其是埋藏改造过程中团簇同位素温度的重置机理;二是将传统的碳、氧同位素指标与新兴的团簇同位素指标相结合,进行多指标的地球化学综合分析,...

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Published in北京大学学报（自然科学版） Vol. 59; no. 6; pp. 1052 - 1068
Main Authors 李世恩, 关平
Format Journal Article
LanguageChinese
Published 造山带与地壳演化教育部重点实验室,北京大学地球与空间科学学院,北京 100871 01.11.2023
Subjects
湖相碳酸盐
clumped isotope
碳、氧同位素
lacustrine carbonate
团簇同位素
carbon and oxygen isotopes
Online AccessGet full text
ISSN0479-8023
DOI10.13209/j.0479-8023.2023.067

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Abstract 总结近年来传统碳、氧同位素及新兴团簇同位素在湖相碳酸盐中的研究进展,梳理湖相环境中碳酸盐同位素组成变化的影响因素及两种同位素方法在地质研究中的应用,探讨当前研究中存在的问题.湖相碳酸盐氧同位素组成受温度的影响较小,主要与湖盆水体的蒸发量和大气降水量有关,碳同位素组成则受湖水蒸发咸化作用以及湖泊有机质与无机质相互作用的共同控制;团簇同位素仅受温度单一因素的影响,是良好的碳酸盐温度计.指出湖相碳酸盐碳、氧同位素研究的两大方向:一是解决团簇同位素理论研究中存在的问题,尤其是埋藏改造过程中团簇同位素温度的重置机理;二是将传统的碳、氧同位素指标与新兴的团簇同位素指标相结合,进行多指标的地球化学综合分析,有效地避免二者在地质研究中的局限性.
AbstractList 总结近年来传统碳、氧同位素及新兴团簇同位素在湖相碳酸盐中的研究进展,梳理湖相环境中碳酸盐同位素组成变化的影响因素及两种同位素方法在地质研究中的应用,探讨当前研究中存在的问题.湖相碳酸盐氧同位素组成受温度的影响较小,主要与湖盆水体的蒸发量和大气降水量有关,碳同位素组成则受湖水蒸发咸化作用以及湖泊有机质与无机质相互作用的共同控制;团簇同位素仅受温度单一因素的影响,是良好的碳酸盐温度计.指出湖相碳酸盐碳、氧同位素研究的两大方向:一是解决团簇同位素理论研究中存在的问题,尤其是埋藏改造过程中团簇同位素温度的重置机理;二是将传统的碳、氧同位素指标与新兴的团簇同位素指标相结合,进行多指标的地球化学综合分析,有效地避免二者在地质研究中的局限性.
Author 李世恩
关平
AuthorAffiliation 造山带与地壳演化教育部重点实验室,北京大学地球与空间科学学院,北京 100871
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LI Shien
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clumped isotope
碳、氧同位素
lacustrine carbonate
团簇同位素
carbon and oxygen isotopes
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