在地幔衍生融化的来源中回收的地的数量
Alexander V Sobolev1, Albrecht W Hofmann, Dmitry V Kuzmin
1Max Planck Institute (MPI) for Chemistry, Post Office Box 3060, 55020 Mainz, Germany. sobolev@geokhi.ru
概括
回收的海洋地 (生态石) 显著影响地幔融化,产生混合型火山石. 橄烯晶分析量化了这种回收的地在各种玄武岩类型和科马提岩中的贡献.
科学领域:
- 地质化学 地质化学
- 石化学 石化学是一门学科.
- 构造学 构造学 构造学 构造学
背景情况:
- 板块构造学将玄武岩海洋地 (生态石) 循环回收到地球的周周地幔中.
- 在地幔融化中,生态石和石对地幔融化的相对贡献并没有得到很好的限制.
研究的目的:
- 为了研究由生态矿衍生的矿和矿之间的相互作用产生的地幔融的化学演变.
- 量化回收的地物质在产生不同类型的地幔融化的比例.
主要方法:
- 分析各种玄武岩石和科马提岩石中橄烯晶体的组成.
- 模拟来自混合型铁石的部分化的化学特征.
主要成果:
- 埃克洛-矿反应产物的部分化物 (混合矿) 富含Ni和Si,但与矿化物相比,Mn,Ca和Mg的含量较低.
- 橄烯晶组成表明,中海基岩 (10-30%),海洋岛屿和大陆基岩 (>60%) 和科马提岩 (20-30%) 中的融贡献显著.
结论:
- 该研究量化了回收地在地幔融化的参与率,从2%到20% (高达28%).
- 橄氨酸晶化学作用是作为一个可靠的追踪器,用于在地幔衍生的岩石中回收的地成分.
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