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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
研究论文     
中国黄土堆积的磁性记录与古降雨量重建
胡蒙育,B. Maher
CentreforEnvironmentalMagnet ismandPalaeomagnetism,DepartmentofGeography,LancasterUniv er si ty,La ncasterLA14YB,UK
THE MAGNETIC RECORDS OF THE CHINESE LOESS-SOIL SEQUENCES AND PALAEORAINFALL RECONSTRUCTION
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)  
摘要:

概述了中国黄土和古土壤堆积的磁性特征,进而介绍成壤作用磁铁矿成因模式,讨论控制黄土—古土壤层矿物磁性特征的气候参量及其利用土壤成因磁化率重建古降雨量。

关键词: 黄土古土壤磁性特征土壤成因磁化率古降雨量    
Abstract:

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: m.hu@lancaster.ac.uk     E-mail: m.hu@lancaster.ac.uk
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: m.hu@lancaster.ac.uk
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引用本文:

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.

HU Meng-yu,Barbara A. Maher. THE MAGNETIC RECORDS OF THE CHINESE LOESS-SOIL SEQUENCES AND PALAEORAINFALL RECONSTRUCTION. Advances in Earth Science, 2002, 17(3): 320-325.

链接本文:

http://www.adearth.ac.cn/CN/10.11867/j.issn.1001-8166.2002.03.0320        http://www.adearth.ac.cn/CN/Y2002/V17/I3/320

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