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东太平洋的岩性岩石上升:性火山套件似乎是从地幔中挤出的一种托莱伊特基岩石中区分出来的
概括
海洋岩基岩是东太平洋起的主要岩,因低含量而与大陆类型不同. 海底山上的性火山套件很可能是通过差异化从这个托莱伊特基岩产生的.
科学领域:
- 大洋火山活动的地球化学和石化学.
- 地幔地质化学和岩起源
背景情况:
- 沿着东太平洋起的火山建筑展示了不同的地化学套房.
- 顶峰地区是性火山岩的宿主,而淹没的部分则由托莱伊特基岩石主导.
研究的目的:
- 描述海洋托莱石和性火山套件之间的地化学差异.
- 调查基岩的起源和底层地幔的组成.
主要方法:
- 来自东太平洋起的火山岩石的地球化学分析.
- 不同火山套件之间的化学成分 (K,P,U,Th,Pb,Ti,SiO2) 的比较.
- 评估主要和微量元素度,以推断岩来源和过程.
主要成果:
- 海洋托莱基岩,K,P,U,Th,Pb和Ti含量较低,是主要的岩类型.
- 性火山套件不那么丰富,并且可能通过差异化从托莱伊特基岩石中衍生出来.
- 独特的化学标准,特别是含量,区分海洋和大陆托莱石.
结论:
- 东太平洋上升下的地幔在和其他微量元素方面已经耗尽.
- 岩分化在从一个共同的岩源产生多样化的火山套件方面发挥着关键作用.
- 建议进行进一步的深度钻探,以研究托莱伊特和类型之间的过渡基岩.
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