探测大量的托巴岩的积累历史
1Department of Earth and Space Sciences, University of California, Los Angeles, CA 90095-1567, USA. jvazquez@ess.ucla.edu
概括
最年轻的托巴塔夫喷发之前有15万年的岩演变. 艾兰石晶体揭示了11万年的停滞期,随后在大规模喷发之前,35,000年的融化多样性不断增加.
科学领域:
- 地质化学 地质化学
- 火山学 火山学是一门学科.
- 同位素地质年代学 同位素地质年代学
背景情况:
- 最年轻的托巴塔夫 (YTT) 喷发代表了地球上最大的四分期火山事件.
- 了解超级喷发之前的长期岩过程对于危险评估至关重要.
研究的目的:
- 重建导致YTT超级喷发的岩过程和时间表.
- 利用艾兰石晶体化学和地质年代学来解读岩储存和演化.
主要方法:
- 来自YTT的艾伦酸盐晶体的化学分析.
- 艾伦石晶体的年代测定,以确定岩演变的时间表.
- 组合区分分析以推断岩性质的变化.
主要成果:
- 艾兰石晶体记录了至少15万年的岩储存和演变.
- 主要的亚火山性岩在约11万年内保持同质性和热性停滞.
- 融化多样性和系统增长的显著增加发生在火山爆发前35,000年.
结论:
- YTT超级喷发是长期的岩积累和以后的快速进化阶段的高潮.
- 艾兰石地质年代学为大型状系统提供了爆发前的岩动态的详细记录.
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