1) palaeomagnetic polar wander
古地磁极移
2) paleomagnetic pole
古地磁极
1.
Paleomagnetic poles of mafic dyke swarms from the North China craton and their relevance to the reconstruction of the supercontinent Columbia.
华北基性岩墙群的古地磁极及其哥伦比亚超大陆重建意义
2.
9° respectively, and the paleomagnetic pole is located at 79.
９°，古地磁极位置北纬７９。
3) geomagnetic polarity offset
地磁极偏移
1.
Paleogeomagnetic age for the middle part of the column of Taiping cave in Guilin is in-ferred based on the Laschamp geomagnetic polarity offset event.
以拉尚（Ｌａｓｃｈａｍｐ）地磁极偏移现象，推测了桂林太平岩洞穴石柱中部的古地磁年龄，并通过分析石柱下部的剩磁方向以及剩磁强度特征，指出该部可能因后期地下水改造而受到现代磁场重磁化。
4) paleomagnetic polarity reverse
古地磁极倒转
1.
Coupling of paleomagnetic polarity reverse with climatic change recoded by magnetostratigraphy in Northern China during Quaternary;
中国北方第四纪磁性地层记录的古地磁极倒转与气候变化耦合关系
5) Paleomagnetic Euler Poles(PEP)
古地磁欧拉极
6) paleo magnetic pole
古磁极
1.
In the way of this principle, the procedure obtaining remanency direction, paleo magnetic pole and paleo latitude has been programmed.
本文介绍了 Halls[1]提出的《根据会聚重磁化圆求剩磁方向的最小二乘法》的原理 ,据此编制了求剩磁方向、古磁极及古纬度的程序。
补充资料：古地磁极移
见古地磁学。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条