期刊文献+
共找到2篇文章
< 1 >
每页显示 20 50 100
Geological Evidence for the Presence of the Emperor Event in China 被引量:2
1
作者 Ge Tongming, Fan Limin and Liu Jian Guangzhou Marine Geological Survey, Ministry of Geology and Mineral Resources of China, Guangzhou 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 1993年第2期235-244,共10页
The presence of the reversals of the geomagnetic field within the Brunhes is indicated by paleomagnetic stuides on Cenozoic volcanic rocks in the Leizhou Peninsula, loess strata and Quaternary marine sediments in the ... The presence of the reversals of the geomagnetic field within the Brunhes is indicated by paleomagnetic stuides on Cenozoic volcanic rocks in the Leizhou Peninsula, loess strata and Quaternary marine sediments in the Pearl River Mouth basin in China. These regional reversals occured at 0.58±0.13 Ma, 0.45 Ma and 0.47—0.48 Ma respectively according to the results of K-Ar isotopic dating and climatostratigraphic and biostratigraphic analyses. The reversals equivalent to the Emperor Event is suggested.The reversals revealed in different regions with various lithologic characters in China prove that the Emperor Event is a global reversal event rather than a geomagnetic excursion, and its confirmation will permit a precise definition of the Middle/Late Pleistocene boundary. 展开更多
关键词 brunhes polarity reversal emperor event
下载PDF
安比拉事件在中国存在的证据 被引量:4
2
作者 葛同明 樊利民 刘坚 《地质学报》 EI CAS CSCD 北大核心 1992年第4期381-389,共9页
黄土地层、珠江口盆地第四纪地层以及雷州半岛英利火山岩的古地磁学研究表明,布容极性时出现有反极性地磁场。英利火山岩的K—Ar同位素年代测定值为0.58±0.13Ma。据气候地层学和生物地层学资料确定,黄土地层和珠江口盆地第四纪地... 黄土地层、珠江口盆地第四纪地层以及雷州半岛英利火山岩的古地磁学研究表明,布容极性时出现有反极性地磁场。英利火山岩的K—Ar同位素年代测定值为0.58±0.13Ma。据气候地层学和生物地层学资料确定,黄土地层和珠江口盆地第四纪地层的反极性层段的年代分别为0.45Ma和0.47—0.48Ma。这些反极性层段的年代相当于安比拉事件的年代。从中国不同地区、不同地层揭示的这一事件证实了安比拉事件为全球性极性倒转,并非极性漂移。安比拉事件的确定将为中、晚更新世地层的划分提供磁极性的依据。 展开更多
关键词 布容极性时 安比拉事件 地磁学
下载PDF
上一页 1 下一页 到第
使用帮助 返回顶部