Paleomagnetism Applied to the Paleozoic Tectonics of China

古生代板块的位置和方向 而构成今天亚洲的岛屿并不为人所知， 但这些信息是古地理和 全球地球物理观点。 该项目将利用 西部新发现的奥陶系和志留系 华北陆块边缘古地磁极的确定 这些人的位置。 结果将有助于解开 中国大地构造史，并提供古地磁参考 确定相对位移和吸积时间的标架 中国境内和境外的街区和街区。

Paleozoic positions and orientations of the cratonic blocks and terranes that constitute present-day Asia are not well known, but this information is required from both paleogeographic and global geophysical stand points. This project will utilize recently-discovered Ordovician and Silurian strata from the western margin of the North China Block to determine paleomagnetic pole positions for these terranes. Results will help unravel the tectonic history of China and provide a paleomagnetic reference frame for determining relative displacements and times of accretion of blocks and terranes both within and outside China.