地磁极 geomagnetic pole
- 对各构造带中的岩石地层进行了古地磁研究与对比,建立了各自的古地磁极移曲线。
Paleomagnetic study and correlation of rocks and strata were conducted in various tectonic belts, and their respective paleomagnetic polar wandering curves were constructed. - 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.
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