概括
对体石的新微探测分析显示,平衡温度较低,约为850°C. 奥利文 - 奥托皮洛克森分区偏离了理想的行为,挑战了先前的估计.
科学领域:
- 地质化学 地质化学
- 矿物学是什么?矿物学是什么?
- 行星科学 行星科学
背景情况:
- 体石提供了关于太阳系早期条件的见解.
- 了解矿物分离对于温度测量至关重要.
研究的目的:
- 计算Fe(++) 和Mg(++) 的分布系数,在共存的火和橄中.
- 为了确定平衡温度,并评估矿物分区的理想行为.
主要方法:
- 利用电子微探针分析,获取有关共存的橄素,正氧氧素和氧素的新数据.
- 为Fe-Mg交换计算的分布系数 (KD).
主要成果:
- 估计平衡温度在850°C左右.
- 在橄素-甲基素Fe-Mg分区中观察到偏离理想行为.
- 与之前的研究相比,确定了明显较低的平衡温度.
结论:
- 850°C的平衡温度为这些体石提供了修订后的热史.
- 在橄烯 - 甲基烯系统中,非理想的混合需要在温度计计算中仔细考虑.
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