花岩的低温结晶和对地岩的影响
Michael R Ackerson1,2, B O Mysen3, N D Tailby4
1Geophysical Laboratory, Carnegie Institution of Washington, Washington, DC, USA. ackerm4@rpi.edu.
Nature
|June 29, 2018
概括
石榴石结晶温度远低于以前的想法,这表明岩体较冷,影响了地球地和矿石沉积形成的模型.
科学领域:
- 地质学
- 石油学
- 地质化学
背景情况:
- 石榴石提供了关于岩火山,大陆形成和地特性的见解.
- 目前的模型表明,花岩在650-700°C或以上的温度下结晶.
- 岩石的结晶温度对于理解各种地质现象至关重要.
研究的目的:
- 为了研究花岩的结晶温度.
- 挑战高岩结晶温度的现有模式.
- 探索花岩结晶温度的影响.
主要方法:
- 分析了来自加利福尼亚州Tuolumne入侵套房的石英晶体.
- 中的石英温度计的应用.
- 使用石英中的度扩散建模.
主要成果:
- 图卢姆尼样本中的石英晶体显示结晶温度为474-561°C.
- 大部分的花岩矿物质结晶在100~200°C以下.
- 超过80%的石英在较低的温度下结晶.
结论:
- 石岩是火山岩的侵入性对应物, 结晶的温度远低于传统所接受的温度.
- 经过修订的花岩结晶温度证实了较冷的岩储存.
- 降低的温度影响了矿矿床的形成和地的热结构.
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