摘要
This paper presents the results of palaeomagnetic studies of Cenozoic volcanic rocks and Quaternary strata in China, which have confirmed the occurence of some short-period polarity events. After a correlation with the worldwide palaeomagnetic data, a geomagnetic polarity time scale for the time since 2.48 M*** has been compiled.
This paper presents the results of palaeomagnetic studies of Cenozoic volcanic rocks and Quaternary strata in China, which have confirmed the occurence of some short-period polarity events. After a correlation with the worldwide palaeomagnetic data, a geomagnetic polarity time scale for the time since 2.48 M*** has been compiled.