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在重新审视已有古地磁研究结果基础上,利用近年来最新研究成果,尤其是早古生代的古地磁数据,建立了扬子地块显生宙古地磁视极移曲线,为研究扬子地块乃至整个中国的大地构造演化提供了新的古地磁依据.
Based on the reexamination of the existing paleomagnetic research results and using the latest research results in recent years, especially the paleomagnetic data of the Early Paleozoic, the paleomagnetic shift curve of the Phanerozoic of the Yangtze block was established. China's tectonic evolution provided a new paleomagnetic evidence.