High temperature measurements of magnetic susceptibility in clay-rich layers

High temperature measurements of magnetic susceptibility in clay-rich layers. Magnetite, characterised by a Curie temperature of 590 °C, dominates the signal.

本数据集针对富黏土层开展磁化率（magnetic susceptibility）的高温测量。其中以590℃的居里温度（Curie temperature）为特征的磁铁矿（magnetite）主导了该测试信号。