首页> 外文期刊>Studia Geophysica et Geodaetica >Indices for Numerical Characterization of the Alteration Processes of Magnetic Minerals Taking Place During Investigation of Temperature Variation of Magnetic Susceptibility
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Indices for Numerical Characterization of the Alteration Processes of Magnetic Minerals Taking Place During Investigation of Temperature Variation of Magnetic Susceptibility

机译:在研究磁化率温度变化过程中发生的磁性矿物蚀变过程数值表征的指标

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The alteration of magnetic minerals taking place during the investigation of the temperature variation of bulk magnetic susceptibility is obvious from different courses of heating and cooling susceptibility vs. temperature curves. A set of indices is introduced to characterize these changes numerically. The A 40 alteration index characterizes the change in susceptibility after executing the whole cycle of heating and cooling. The maximum difference between the heating and cooling curves is characterized by the A max alteration index. The mean or average difference between the heating and cooling curves is characterized by the A m alteration index. The situation whether the heating and cooling curves cross, is characterized by the A cr alteration index. The technique of progressive repeated heating is proposed, together with the above indices, to locate the temperature intervals with weak and strong magnetic mineral changes induced by heating.
机译:从不同的加热和冷却磁化率对温度曲线的变化过程来看,在研究大块磁化率温度变化过程中发生的磁性矿物的变化是显而易见的。引入一组索引以数字方式表征这些变化。 A 40 的变化指数表示在执行整个加热和冷却循环后磁化率的变化。加热曲线和冷却曲线之间的最大差异由A max 改变指数表征。加热曲线和冷却曲线之间的平均差或平均差由A m改变指数表征。加热曲线和冷却曲线是否交叉的情况以A cr 改变指数为特征。提出了逐步重复加热的技术,并结合上述指标,以定位加热引起的弱磁性和强磁性矿物变化的温度区间。

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