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地球科学进展  2002, Vol. 17 Issue (3): 320-325    DOI: 10.11867/j.issn.1001-8166.2002.03.0320
胡蒙育,B. Maher
CentreforEnvironmentalMagnet ismandPalaeomagnetism,DepartmentofGeography,LancasterUniv er si ty,La ncasterLA14YB,UK
HU Meng-yu,Barbara A. Maher
Centre for Environmental Magnetism and Palaeomagnetism,Department of Geography,Lancaster University, Lancaster LA1 4YB, UK
 全文: PDF(78 KB)  


关键词: 黄土古土壤磁性特征土壤成因磁化率古降雨量    

This paper outlines the magnetic properties of the Chinese loess-palaeosol sequences and introduces the model of pedogenic magnetite formation. It further discusses the correlation between rainfall and pedogenic susceptibility and the approaches to palaeoclimate reconstruction.

Key words: Loess    Palaeosol    Magnetic properties    Pedogenic susceptibility    Palaeorainfall.
收稿日期: 2001-05-08 出版日期: 2002-06-01
:  P539   
通讯作者: 胡蒙育(1956-),男,河北定州人,博士,主要从事古地磁与环境磁学研究.E-mail:     E-mail:
作者简介: 胡蒙育(1956-),男,河北定州人,博士,主要从事古地磁与环境磁学研究.E-mail:
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胡蒙育,B. Maher. 中国黄土堆积的磁性记录与古降雨量重建[J]. 地球科学进展, 2002, 17(3): 320-325.



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