在冷藏库中保存的岩晶体的快速移动
Kari M Cooper1, Adam J R Kent2
1Department of Earth and Planetary Sciences, University of California, Davis, One Shields Avenue, Davis, California 95616, USA.
Nature
|February 18, 2014
概括
了解岩储存是火山学的关键. 新的方法揭示了大多数岩在高温中花费的时间很少,这表明从较冷的状态迅速调动爆发之前的爆发.
科学领域:
- * 火山学和岩石学.
- * 地质化学和地质年代学.
- *地球科学和岩动力学.
背景情况:
- * 岩储存和重新调动过程对于理解火山爆发至关重要.
- * 岩水库的物理条件和热史尚不清楚.
- * 关于岩是否需要高温或接近固体的储存来调动存在争论.
研究的目的:
- * 开发一种制约岩水库热史的方法.
- * 通过使用晶体特性,将热条件与储存时间表联系起来.
- * 调查胡德山和其他火山的岩储存条件.
主要方法:
- * 联合系列不平衡,晶体大小和微量元素划分.
- *分析了水晶数据,以推断岩的热史.
- * 适用于美国俄勒冈州胡德山样本的方法.
主要成果:
- * 胡德山的岩在临界结晶度 (40-50%) 以上的时间是最小的 (可能为<1%).
- * 在不同的火山系统中,低温储存似乎很普遍.
- *温度计可能反映结晶,而不是长期储存条件.
结论:
- * 快速调动接近固态的岩是一种常见的过程.
- * 岩储存主要发生在较低的温度下.
- *可检测到的,主要是液态的岩体可能表明即将发生的喷发.
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