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New insights into the palaeoclimatic interpretation of the temperature dependence of the magnetic susceptibility and magnetization of Mid-Late Pleistocene loess/palaeosols in Central Asia and the Chinese Loess Plateau
Zan, JB (Zan, Jinbo)1,2; Fang, XM (Fang, Xiaomin)2; Yan, MD (Yan, Maodu)2; Li, BS (Li, Bingshuai)2; Zan, JB
Source PublicationGEOPHYSICAL JOURNAL INTERNATIONAL
2017
Volume208Issue:2Pages:663-673
DOI10.1093/gji/ggw419
AbstractThe temperature dependence of magnetic susceptibility (chi-T curves) and magnetization (M-T curves) has been used as a routine rock magnetic tool to characterize the magnetic mineralogy and magnetic granulometry of Chinese loess/palaeosols. However, palaeoclimatic interpretation of these thermomagnetic analyses remains controversial. In the present study, total organic carbon (TOC), thermomagnetic and low-temperature magnetic experiments on Mid-Late Pleistocene loess/palaeosols in Central Asia and the Chinese Loess Plateau (CLP) have been conducted. We found that the M (T) cooling curves at room temperature were mostly lower than the corresponding heating curves, whereas for the chi(T) analyses the cooling curves at room temperature were always much higher than the heating curves. Low-temperature magnetic measurements demonstrated that a large amount of superparamagnetic ferrimagnetic particles were produced during the thermal treatment and resulted in the aforementioned differences. This finding further indicated that the use of the M-T curves to estimate the relative content of maghemite in the loess/palaeosols from the CLP was problematic. In addition, a positive correlation exists between the TOC and the frequency-dependent susceptibility (chi(FD)) in the CLP, suggesting that stronger pedogenesis would result in the simultaneous increase in the content of both maghemite and organic matter. Consequently, the parameters Delta chi(1) (representing the relative content of pedogenic maghemite), Delta chi(2) (inverted left perpendicular chi(ph) - chi- inverted right perpendicular] + Delta chi(1)) and chi(ph) (related to the organic matter concentration), which can be calculated from the chi-T analyses, can potentially be used as new indicators of pedogenesis and palaeoclimate in Central Asia and the CLP.
Subject Area地质学
WOS IDWOS:000396817600005
Language英语
Indexed BySCI
KeywordSIZE DISTRIBUTION DEPOSITS PEDOGENESIS MAGHEMITE SEQUENCE ORIGIN
WOS Research AreaGeochemistry & Geophysics
WOS SubjectGeochemistry & Geophysics ; Geochemistry & Geophysics
Cooperation Status国内
SubtypeArticle
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Document Type期刊论文
Identifierhttp://ir.itpcas.ac.cn/handle/131C11/8222
Collection图书馆
Corresponding AuthorZan, JB
Affiliation1.Chinese Acad Sci, CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China.
2.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Continental Collis & Plateau Uplift, Beijing 100101, Peoples R China.
Recommended Citation
GB/T 7714
Zan, JB ,Fang, XM ,Yan, MD ,et al. New insights into the palaeoclimatic interpretation of the temperature dependence of the magnetic susceptibility and magnetization of Mid-Late Pleistocene loess/palaeosols in Central Asia and the Chinese Loess Plateau[J]. GEOPHYSICAL JOURNAL INTERNATIONAL,2017,208(2):663-673.
APA Zan, JB ,Fang, XM ,Yan, MD ,Li, BS ,&Zan, JB.(2017).New insights into the palaeoclimatic interpretation of the temperature dependence of the magnetic susceptibility and magnetization of Mid-Late Pleistocene loess/palaeosols in Central Asia and the Chinese Loess Plateau.GEOPHYSICAL JOURNAL INTERNATIONAL,208(2),663-673.
MLA Zan, JB ,et al."New insights into the palaeoclimatic interpretation of the temperature dependence of the magnetic susceptibility and magnetization of Mid-Late Pleistocene loess/palaeosols in Central Asia and the Chinese Loess Plateau".GEOPHYSICAL JOURNAL INTERNATIONAL 208.2(2017):663-673.
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