摘要
Extensive paleomagnetic studies in the Yangtze Block of South China has been performed since the 1980s, and the Phanerozoic APW (apparent polar wander)path has been established based on a large amount of data obtained. However, the Huanan Block in southeastern region still remains unknown paleomagnetically. In order to further understand the plate tectonic patterns and evolutional history prio Mesozoic collision of the
基金
Project supported dually by the National Natural Science Foundation of China and Swiss Federal Institute of Technology ,Zurich
