在10-50°C时测量石的地热量
Gabriella Koltai1, Tobias Kluge2,3, Yves Krüger4
1Institute of Geology, University of Innsbruck, Innrain 52, 6020, Innsbruck, Austria. gabriella.koltai@uibk.ac.at.
Scientific reports
|January 18, 2024
概括
准确测量低温石的形成是具有挑战性的. 这项研究验证了多种地热测量方法,发现晶体形状可以在地热和天热系统中定性地指示温度.
科学领域:
- 地质化学 地质化学
- 矿物学是什么?矿物学是什么?
- 地热度测量 (Geothermometry) 是一种测量方法.
背景情况:
- 碳酸盐地热测量对于理解地热和地化学系统至关重要.
- 对于低温石 (低于40-60°C) 进行准确的温度测定是很困难的.
- 现有的方法需要验证,以准确的低温评估.
研究的目的:
- 对低温石进行三种地热度测量方法 (Δ47温度测量,核化辅助液体入微热度测量[NA-FIM]和氧同位素温度测量) 的交叉验证.
- 评估这些方法的准确性和精度到10°C.
- 调查石晶体形态与形成温度之间的关系.
主要方法:
- 用Δ47-温度计对水下石样本的应用.
- 使用核化辅助的液体纳入微热法 (NA-FIM).
- 在含有初级流体含有样品上使用氧同位素温度计.
主要成果:
- 对于大多数样本,NA-FIM和Δ47-温度计在95%的置信区间内显示出一致.
- 回归分析表明,在10-50°C范围内的Δ47-温度计的实际不确定性为±6.6°C.
- 石晶体形态与温度相关:的圆柱体 (<13°C),的圆柱体 (10-29°C) 和圆柱体 (>30°C).
结论:
- 对于低温石地热量测量,Δ47-温度计和NA-FIM可靠,而Δ47-温度计的实际不确定性高于分析估计.
- 氧同位素温度计为一些样本提供了一致的结果,但由于包含可用性而受到限制.
- 石晶体形态为区分低温 (<30°C) 和高温石形成提供了定性指标.
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