论文部分内容阅读
由于非滞后剩磁各向异性和等温剩磁各向异性的参数直接与岩石中的携磁矿物颗粒有关，它比传统的磁化率各向异性更明确地指示岩石组构，在构造地质研究中有较大应用前景．本文介绍了非滞后剩磁及其各向异性的测定方法，并以一个实例阐述了它在构造地质中的应用．
Since the parameters of non-hysteretic remanent anisotropy and isothermal remanent magnetisotropy are directly related to the magnetic bearing mineral grains in the rock, it is more specific than the traditional magnetic susceptibility anisotropy to indicate rock structure. In the study of structural geology Have greater application prospects. In this paper, the measurement method of non-hysteresis remanence and its anisotropy is introduced and an example is given to illustrate its application in structural geology.