概括
西伯利亚陷,一个巨大的洪水玄武岩形成,在900,000多年内迅速爆发,从24.8亿年前开始,这表明地幔羽毛起源. 这种火山活动与二叠纪-三叠纪大规模灭绝相吻合,使其因果关系不确定.
科学领域:
- 地质科学是地球科学.
- 火山学 火山学是一门学科.
- 古生物学的古生物学
背景情况:
- 西伯利亚陷是地球上最大的洪水玄武岩地区之一.
- 了解它们的喷发动态是理解大规模火山事件的关键.
研究的目的:
- 为了准确地确定西伯利亚陷喷发的日期.
- 为了确定喷发率和潜在原因.
- 为了研究与二叠纪-三叠纪大灭绝的时间关系.
主要方法:
- 激光加热 (40) Ar/(39) Ar 地质年代学被用来测定基岩的年代.
- 喷发率是根据其体积和持续时间来计算的.
- 评估了关于岩层裂纹的地质背景.
主要成果:
- 大多数西伯利亚陷玄武岩都在短短的90万+/-80万年间爆发.
- 喷发开始于大约2.48亿年前,其速度超过1.3公里3/年.
- 火山活动与显著的石质层裂变没有联系,质疑解压融化是主要的驱动因素.
结论:
- 高的喷发率支持西伯利亚陷的地幔羽毛模型.
- 由于石质层裂变而导致地幔减压可能不是化的主要原因.
- 西伯利亚陷火山活动的时间与珀米亚-三叠纪大灭绝密切相关,但直接的因果关系仍然是一个开放的问题.
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