摘要
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 inclination 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 principles and cases,this paper summarizes the general process of correction shallow bias of inclination in the sedimentary rocks.
出处
《重庆科技学院学报(自然科学版)》
CAS
2017年第6期26-29,共4页
Journal of Chongqing University of Science and Technology:Natural Sciences Edition
基金
高等学校博士学科点专项科研基金项目"藏北雁石坪地区中-晚侏罗世沉积地层的古地磁学研究"(20136101120005)
关键词
沉积岩
磁倾角浅化
E/I法
非滞后剩磁各向异性法
等温剩磁各向异性法
sedimentary rock
shallowbias of inclination
E / I method
anisotropy of anhysteretic remant magneti-zation
anisotropy of isot!iemial remanent magnetism