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中国黄土堆积的磁性记录与古降雨量重建
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. DOI: 10.11867/j.issn.1001-8166.2002.03.0320
作者姓名:胡蒙育  B.Maher
作者单位:[1]CentreforEnvironmentalMagnetismandPalaeomagnetism,DepartmentofGeography,LancasterUniversity,LancasterLA14YB,UK [2]CentreforEnvironmentalMagnetismandPalaeomagnetism,DepartmentofGeography,LancasterUniversi
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
文章编号:1001-8166(2002)03-0320-06
收稿时间:2001-05-08
修稿时间:2001-05-08

THE MAGNETIC RECORDS OF THE CHINESE LOESS-SOIL SEQUENCES AND PALAEORAINFALL RECONSTRUCTION
HU Meng yu,Barbara A. Maher. THE MAGNETIC RECORDS OF THE CHINESE LOESS-SOIL SEQUENCES AND PALAEORAINFALL RECONSTRUCTION[J]. Advances in Earth Sciences, 2002, 17(3): 320-325. DOI: 10.11867/j.issn.1001-8166.2002.03.0320
Authors:HU Meng yu  Barbara A. Maher
Affiliation:Centre for Environmental Magnetism and Palaeomagnetism,Department of Geography,Lancaster University, Lancaster LA1 4YB, UK
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.
Keywords:Loess  Palaeosol  Magnetic properties  Pedogenic susceptibility  Palaeorainfall
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