南京下蜀土剖面磁化率测量及其与深海沉积的对比  

THE MAGNETIC SUSCEPTIBILITY MEASUREMENT OF XIASHU LOESS SECTION NEAR NANJING AND CORRELATION WITH THE RECORDS OF DEEP-SEA SEDIMENTS

作　　者：许峰宇[1] 李立文[2] 

机构地区：[1]徐州师范学院地理系 [2]南京师范大学

出　　处：《江苏师范大学学报（自然科学版）》1992年第1期22-26,共5页Journal of Jiangsu Normal University：Natural Science Edition

基　　金：国家自然科学基金

摘　　要：本文通过对典型样品的低温磁行为分析探讨了磁化率反映古气候的机制,并尝试把下蜀土剖面磁化率古气候记录与华北黄土及深海沉积的记录相对比。The Xinshengwei section of Xiashu loess which was discovered recently is a more successive section near Nanjing. The magnetic susceptibility measurements of the section show that the alternation of crest and trough on the magnetic susceptibility currle of the section has close relation with the soil-loess sequence, and the cause has been probed into by the analysis of the behavior of the typical samples. The characteristic of the climatic evolution in the region has been posed by the comparison between the paleo-climatic records of Nanjing loess, Central China loess and the deep-sea sediments.

关 键 词：下蜀土 古土壤 磁化率 

分 类 号：N55[自然科学总论]