古地磁

Paleomagnetic studies have provided valuable insights into the Earth's past.
古地磁研究为地球的过去提供了有价值的见解。
The data from paleomagnetic studies are crucial for understanding plate tectonics.
古地磁研究的数据对于理解板块构造至关重要。
The alignment of magnetic minerals in rocks can be used to determine the paleomagnetic pole.
岩石中磁性矿物的排列可用于确定古地磁极。
Paleomagnetism has been instrumental in reconstructing the history of the Earth's magnetic field.
古地磁在重建地球磁场的历史中起到了关键作用。
Scientists use paleomagnetic data to correlate rock formations from different geographic locations.
科学家使用古地磁数据来关联来自不同地理位置的岩石层。
The study of paleomagnetism helps in understanding the movement of continents over geological time.
古地磁学的研究有助于了解大陆在地质时间中的移动。
Paleomagnetic anomalies can indicate the presence of ancient magnetic materials in the Earth's crust.
古地磁异常可以表明地壳中有古代磁性物质的存在。
The measurement of the Earth's past magnetic field strength is possible through paleomagnetic analysis.
通过古地磁分析，可以测量地球过去磁场的强度。
The field of paleomagnetism overlaps with other disciplines such as geology, archaeology, and paleontology.
古地磁学与地质学、考古学和古生物学等其他学科重叠。
The discovery of reversals in the Earth's magnetic field was made possible by paleomagnetic research.
古地磁研究使我们能够发现地球磁场反转的现象。