青藏高原东南缘甘孜黄土磁化率揭示的西南季风演化

以青藏高原东南缘甘孜A剖面黄土-古土壤序列为材料,在磁性地层学研究的基础上,对其高分辨率磁化率记录的多时间尺度气候特征进行了分析。磁性地层学研究结果表明,甘孜A剖面典型风尘堆积的底界年龄约为1.16 Ma。磁化率记录在构造时间尺度上具有明显的阶段性,显示了西南季风演化存在中更新世气候转型。功率谱分析检出典型的偏心率100 ka、斜率41 ka、岁差23 ka轨道周期和11.4、7.5 ka的岁差拍頻周期,指示西南季风演化受天文因素影响,印度季风系统对太阳辐射具有非线性响应和热带特征。...

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Published inHăiyang dĭzhĭ yu dĭsĭjĭ dĭzhĭ Vol. 29; no. 5; p. 115
Main Authors LIU, Dongyan, Shasha, PENG, QIAO Yansong, XIE Ruihuang
Format Journal Article
LanguageChinese
Published Beijing Marine Geology and Quaternary Geology 01.01.2009
Subjects
Beat frequencies
Earth orbits
Evolution
Loess
Magnetic permeability
Magnetic susceptibility
Magnetostratigraphy
Monsoons
Nonlinear response
Paleosols
Pleistocene
Precession
Sequencing
Spectral analysis
Spectrum analysis
Tibetan Plateau
Online AccessGet full text
ISSN0256-1492
DOI10.3724/SP.J.1140.2009.05115

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Abstract 以青藏高原东南缘甘孜A剖面黄土-古土壤序列为材料,在磁性地层学研究的基础上,对其高分辨率磁化率记录的多时间尺度气候特征进行了分析。磁性地层学研究结果表明,甘孜A剖面典型风尘堆积的底界年龄约为1.16 Ma。磁化率记录在构造时间尺度上具有明显的阶段性,显示了西南季风演化存在中更新世气候转型。功率谱分析检出典型的偏心率100 ka、斜率41 ka、岁差23 ka轨道周期和11.4、7.5 ka的岁差拍頻周期,指示西南季风演化受天文因素影响,印度季风系统对太阳辐射具有非线性响应和热带特征。
AbstractList 以青藏高原东南缘甘孜A剖面黄土-古土壤序列为材料,在磁性地层学研究的基础上,对其高分辨率磁化率记录的多时间尺度气候特征进行了分析。磁性地层学研究结果表明,甘孜A剖面典型风尘堆积的底界年龄约为1.16 Ma。磁化率记录在构造时间尺度上具有明显的阶段性,显示了西南季风演化存在中更新世气候转型。功率谱分析检出典型的偏心率100 ka、斜率41 ka、岁差23 ka轨道周期和11.4、7.5 ka的岁差拍頻周期,指示西南季风演化受天文因素影响,印度季风系统对太阳辐射具有非线性响应和热带特征。
Author LIU, Dongyan
QIAO Yansong
XIE Ruihuang
Shasha, PENG
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Snippet 以青藏高原东南缘甘孜A剖面黄土-古土壤序列为材料,在磁性地层学研究的基础上,对其高分辨率磁化率记录的多时间尺度气候特征进行了分析。磁性地层学研究结果表明,甘孜A剖面典型风尘堆积的底界年龄约为1.16...
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StartPage 115
SubjectTerms Beat frequencies
Earth orbits
Evolution
Loess
Magnetic permeability
Magnetic susceptibility
Magnetostratigraphy
Monsoons
Nonlinear response
Paleosols
Pleistocene
Precession
Sequencing
Spectral analysis
Spectrum analysis
Title 青藏高原东南缘甘孜黄土磁化率揭示的西南季风演化
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