沉积过程中的深度碳循环被石中共存的钻石-甲-石所揭示
Xiaoxia Wang1, Yilin Xiao1,2, Hans-Peter Schertl3
1CAS Key Laboratory of Crust-Mantle Materials and Environments, School of Earth and Space Sciences, University of Science and Technology of China, China.
National science review
|September 6, 2023
概括
沉浮板块释放的碳可以以钻石,甲和磁石的形式储存在地球深处. 这一发现揭示了地幔中深层碳循环的关键机制.
科学领域:
- 地质化学 地质化学
- 矿物学是一门学科.
- 构造学 构造学 构造学 构造学
背景情况:
- 深层碳循环对于调节地球气候和地质活动至关重要.
- 了解地幔中的碳储存对于理解俯冲区过程至关重要.
研究的目的:
- 为了研究碳的储存机制,从覆盖着的地幔中从潜水板中释放的碳.
- 为了确定负责在深处封存碳的矿物阶段.
主要方法:
- 在石样本中分析多相含物.
- 采石和微分析技术来确定包含成分.
主要成果:
- 在石中发现了含有钻石,甲和石的多相内含物.
- 这些插入表明在地幔中存在碳储存储库.
结论:
- 从引板中释放的碳可以作为地幔中钻石,甲和石储存.
- 这个过程代表了深度碳循环的重要途径.
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