在沉积岩的古地磁数据统计中,记录的磁倾角数据普遍存在浅化现象.通过综合分析E/I法、非滞后剩磁各向异性法和等温剩磁各向异性法原理及其研究实例,总结沉积岩磁倾角校正浅化的一般流程.%In the study of paleomagnetism data from sedimentary rocks,we found that there is a shallow bias of in-clination which was recorded by sedimentary rocks generally. Based on the comprehensive analysis of E/I method, the anisotropy of anhysteretic remant magnetization,anisotropy of isothermal remanent magnetism,and their princi-ples and cases,this paper summarizes the general process of correction shallow bias of inclination in the sedimenta-ry rocks.
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