一个快速的机制来重新调动和同质化高度结晶的岩体
Alain Burgisser1, George W Bergantz
1Institut des Sciences de la Terre d'Orléans, CNRS/INSU, Université d'Orléans, 45071 Orléans cedex 2, France. burgisse@cnrs-orleans.fr
Nature
|March 4, 2011
概括
一个新的模型解释了粘性岩系统如何快速混合和同质化,形成大型火山体和火山爆发. 这种"解开"过程涉及重新加热和重新调动富含晶体的岩石.
科学领域:
- 地球科学 地球科学 地球科学
- 地质地质地质地质地质地
- 火山学 火山学是一门学科.
背景情况:
- 大型岩体表现出大规模的同质性和小规模的异质性.
- 现有的模型很难解释粘性,富含晶体的岩石中的快速混合.
研究的目的:
- 提出一种统一的机制来解释岩系统中矛盾的观察结果.
- 通过一个动态模板来证明结晶丰富的 magma 的快速重新调动.
主要方法:
- 开发一个两阶段的动态模型,用于岩的重新调动 ("解压").
- 对再加热,结晶性降低和浮性层形成的分析.
- 模型输出与历史喷发数据 (皮纳图博,蒙塞拉特) 的比较.
主要成果:
- "解"模型成功地解释了岩材料的快速翻转和混合.
- 该模型解释了不同年龄和化学区分的材料的并置.
- 计算的解压速率与历史喷发中观察到的速率一致.
结论:
- "解"机制为大规模的岩现象提供了统一的解释.
- 这一过程对于理解冥子形成 (地形成) 和大型火岩喷发至关重要.
- 该模型在历史数据上的成功证实了其适用于多种不同的岩系统的有效性.
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