概括
火山弧喷发的石与深层地幔过程有关. 安德西特火山活动的岩生成与中等深度地震和贝尼奥夫地震区有关.
科学领域:
- 地质地质地质地质地质地
- 火山学 火山学是一门学科.
- 地震学 地震学
背景情况:
- 环太平洋的石,玄武岩和石从岛屿弧和大陆范围喷发出来.
- 火山弧位置与沟附近的浅地震带相关.
研究的目的:
- 为了研究环太平洋岩火山的地下起源.
- 为了将火山活动与地震数据和地幔结构相关联.
主要方法:
- 火山弧和地震区域的地质测绘.
- 对喷发的岩组成的分析,特别是含量.
- 地震断层扫描用于划定地下结构,如贝尼奥夫区和低速度区域.
主要成果:
- 活火山在地下区域上方排列,由相交的贝尼奥夫区和古登伯格低速区定义.
- 岩中的含量与贝尼奥夫区的深度之间存在着很强的相关性.
- 安德西特火山活动似乎起源于地幔.
结论:
- 安德西特火山活动与地幔过程有关.
- 贝尼奥夫带中介焦点深度的地震事件与岩生成有关.
- 贝尼奥夫带的深度影响了喷发的岩的组成.
相关概念视频
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