相关实验视频
Updated: Jul 12, 2026

11:32
High Pressure Single Crystal Diffraction at PX^2
Published on: January 16, 2017
概括
铁-正氧素的秩序-障碍过渡在480-1000°C之间迅速发生. 研究这些矿物转变揭示了火山岩的冷却速度,特别是在600-480°C之间.
科学领域:
- 矿物学是什么?矿物学是什么?
- 地质化学 地质化学
- 热力学是一种热力学.
背景情况:
- 构成 (Fe,Mg) SiO3 的矿物质奥尔托皮洛,表现出涉及铁和的秩序-混乱过渡.
- 这些过渡对于理解地质材料的热史至关重要.
研究的目的:
- 为了研究orthopyroxenes中秩序-混乱过渡的动力学.
- 为了确定铁矿场占用率和火山岩石冷却率之间的关系.
主要方法:
- 实验研究在骨质皮质素的订制和扰乱过程.
- 在快速冷却的火山样本中分析了转移稳定的铁位占用率.
主要成果:
- 整形素的秩序-乱过渡在大约480°C至1000°C的温度范围内迅速发生.
- 来自火山岩的正氧化素中转移稳定的铁位占用率与它们的冷却速度直接相关.
结论:
- 实验性测定铁矿场占用率为估计火山岩的冷却速度提供了一种可靠的方法.
- 这种方法对于限制冷却在600°C和480°C之间特别有效,这是维护超稳定状态的关键范围.
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08:55Methods of Ex Situ and In Situ Investigations of Structural Transformations: The Case of Crystallization of Metallic Glasses
Published on: June 7, 2018
11:50Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
Published on: June 13, 2015
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