概括
大规模的大陆洪水玄武岩喷发与深层地幔羽毛相关,大型事件代表羽毛头和持续的热点代表羽毛尾. 这个模型解释了火山活动而不需要大陆裂.
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.
- 地质物理学 地质物理学
背景情况:
- 大陆洪水岩喷发会产生大量的岩积累.
- 这些事件经常与主要热点的初始阶段相吻合.
- 理论上,热点源于地幔深层的羽毛.
研究的目的:
- 为了解释洪水玄武岩和热点之间的关系.
- 提出一个地幔羽毛启动及其火山后果的模型.
主要方法:
- 基于相对融体积的模型开发.
- 对喷发率的分析.
- 检查洪水玄武岩和热点的时间和空间关系.
主要成果:
- 洪水玄武岩代表了地幔羽毛的最初"头部".
- 热点代表了持续的"尾巴"或管道的羽毛.
- 该模型考虑了融化量和喷发率.
结论:
- 地幔羽毛启动为洪水玄武岩和热点提供了一个统一的模型.
- 大陆裂不是洪水玄武岩火山活动的先决条件.
- 洪水玄武岩省份可以在海洋和大陆环境中形成.
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