高氧化板内基岩和深层储存碳的高氧化基岩
Xu-Han Dong1, Shui-Jiong Wang1,2, Wenzhong Wang3,4,5
1State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences (Beijing), Beijing 100083, China.
Science advances
|August 7, 2024
概括
在地球深处的再生碳酸盐氧化地幔岩石,储存大量的碳. 在地幔过渡区的停滞不前的浮板是这种深层碳储存和气候调节的关键.
科学领域:
- 地质化学 地质化学
- 地质地质地质地质地质地
- 地球科学 地球科学 地球科学
背景情况:
- 深层碳循环对于地球地幔的动态和可居住性至关重要.
- 回收碳酸盐在地幔氧化还原反应中充当氧化剂,形成氧化域,并在地球深处储存碳.
- 了解这些过程对于理解全球碳循环和气候调节至关重要.
研究的目的:
- 为了研究高度氧化的地幔领域的起源.
- 探索再生碳酸盐在深层碳储存中的作用.
- 为了评估沉积板块对地幔氧化和气候的影响.
主要方法:
- 分析来自中国东部的代内板基岩中高Fe3+/Fe值.
- 基岩样本的地球化学和同位素分析.
- 对地幔氧化还原反应和碳储存的建模.
主要成果:
- 高Fe3+/Fe值在Cenozoic内板基岩中被观察到,表明氧化地幔来源.
- 地质化学和同位素特征表明碳化融与回收碳酸盐组件的参与.
- 证据表明,来自地幔过渡区中停滞不前的沉降板块的氧化地幔领域.
结论:
- 来自停滞不前的沉降板块的碳化融会氧化地幔,产生高度氧化的域.
- 深层地幔的碳储存通过碳-铁氧化还原反应中钻石的形成和分离而得到增强.
- 在地幔过渡区中停滞不前的沉积板块的体积是影响全球气候调节的重要因素.
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