中国第四纪黄土

中国第四纪黄土地球化学研究进展

Progress in geochemical research on the Loess and other Quaternary deposits in China

中国第四纪黄土，以广泛的分布性、沉积的连续性和对全球环境变化事件和古气候演变反应的敏感性，在第四纪古环境研究中具有重大意义。

Loess deposition in China is widely distributed , continuously deposited and sensitively responded to paleo-environment and paleoclimate changes . So it is of great theoretic significance to study loess in Quaternary research .

应用古地磁学原理，分析了中国北方第四纪黄土、泥河湾盆地、黄海陆架磁性地层记录的古地磁极倒转与气候变化之间的关系。

This paper analyzed the relationship between paleomagnetic polarity reverse and climatic change recoded by magnetostratigraphy of loess , Nihewan Basin and Yellow Sea shelf in Northern China during Quaternary by paleomagnetism .

中国西北地区晚第四纪黄土中镁铝地球化学与古气候意义

The Geochemistry and Paleoclimate Significance of Magnesium and Aluminium in Loess of Late Quaternary in Northwestern China