古地磁极

滇东早第三纪的古地磁极位置及磁性地层特征

A case study of the Eogene paleomagnetic pole sites and characteristics of magnetic strata in eastern yunnan , China

华北地块中元古代杨庄组的古地磁研究提供了一个同时通过褶皱检验和倒转检验的古地磁极，极位置为经度190.4°、纬度2.4°。

A high-quality paleomagnetic pole with positive fold and reversal tests at 190.4 ° E , 2.4 ° N has been acquired from the Mesoproterozoic Yangzhuang Formation in North China Block .

利用裂变径迹法测定了济阳坳陷第三系馆陶组至孔店组碎屑沉积岩的年龄，并将所测年龄与古地磁极性年龄、K-Ar法同位素年龄相对比，三者基本一致。

The age of clastic sedimentary rock of the Tertiary Guantao formation to Kongdian for - mation in the Jiyang sag was determined by using the method of fission track and compared with those ages determined by palaeo-geomagnetic polarity and K-Ar isotope , the results were almost the same .

牙形石的三个繁盛期与古地磁极性倒转有关。

Three prosperous periods of conodont have relation to Palaeomagnetism Reversal .

新疆塔里木地台晚古生代古地磁极移曲线及其地质构造含义

Late Paleozoic polar wander path for the Tarim block and tectonic significance

因而，第四纪古地磁极倒转可能是第四纪气候冷暖波动变化的主要驱动因素之一。

Therefore , paleomagnetic polarity reverse of Quaternary may be one of the main driving factors .

华北和华南块体古生代至中生代古地磁极移曲线与古纬度的分布变化峰峰煤田煤质分布变化规律的研究

Revised and Synthetic Apparent Polar Wander Paths of The North and South China Blocks From the Cambrian to Cretaceous The Law Governing Coal Quality Variation Relying on Its Distribution in Fengfeng Coal Field

应用古地磁学原理，分析了中国北方第四纪黄土、泥河湾盆地、黄海陆架磁性地层记录的古地磁极倒转与气候变化之间的关系。

This paper analyzed the relationship between paleomagnetic polarity reverse and climatic change recoded by magnetostratigraphy of loess , Nihewan Basin and Yellow Sea shelf in Northern China during Quaternary by paleomagnetism .