摘要
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．
Rock anisotropy of magnetic remanence refers to anisotropy of anhysteretic remanence and anisotropy of isothermal remanence, which are recently developed techniques for rock fabric study. They are more clear and definite than conventional anisotropy of magnetic susceptibility. The paper introduces the concept of anhysteretic remanence and the method to measure its anisotropy. One case studies were cited to show the application in tectonics.
出处
《地球物理学报》
SCIE
EI
CAS
CSCD
北大核心
1999年第4期572-576,共5页
Chinese Journal of Geophysics
基金
国家自然科学基金!49574216
关键词
非滞后剩磁
各向异性
古地磁
构造演化
Anisotropy of anhysteretic magnetic remanence, Jiangshao collision zone, Paleomagnetism,Tectonic evolution
