The Experts below are selected from a list of 525 Experts worldwide ranked by ideXlab platform

Yan Jun - One of the best experts on this subject based on the ideXlab platform.

  • Can the magnetic susceptibility record of Chinese Red Clay sequence be used for palaeomonsoon reconstructions?
    'Oxford University Press (OUP)', 2016
    Co-Authors: Zhao Guoyong, Han Yan, Liu Xiuming, Chang Liao, Lü Bin, Qu Chen, Guo Xuelian, Yan Junhui, Yan Jun
    Abstract:

    Red Clay underlying the loess-palaeosol sequences on the Chinese Loess Plateau is an Eolian Deposit. There is a controversy over whether magnetic susceptibility (χ) variations in Red Clay sequence can be used as an indicator of summer palaeomonsoon intensity. This study investigates the magnetic mineralogy, magnetic concentration and magnetic grain size distribution of Jiaxian Red Clay with multimagnetic methods. Our results indicate that the magnetic properties of Jiaxian Red Clay are similar to those of the Quaternary loess-palaeosol sequences, and ultrafine ferrimagnetic grains produced during pedogenesis are responsible for an increase in susceptibility, therefore the χ enhancement mechanism of Red Clay is similar to that of the overlying loess-palaeosol sequences. This paper explores χ variations in the Red Clay sequence through spatial and temporal analysis. The susceptibility variation of six sites along a NNE to SSW transect correlate to palaeoclimatic cycles, so χ can be used to trace the summer palaeomonsoon intensity from a spatial perspective. However, a simple loess-derived calibration function cannot be used to quantitative reconstruct the palaeomonsoon intensity variations thought time. An adjusted calibration function for palaeosols from Red Clay sequence needs to be developed, so that χ can be used to quantitative reconstruct palaeomonsoon intensity. Further study is necessary to develop such a transfer function.9 page(s

  • Can the magnetic susceptibility record of Chinese Red Clay sequence be used for palaeomonsoon reconstructions?
    GEOPHYSICAL JOURNAL INTERNATIONAL, 2016
    Co-Authors: Zhao Guoyong, Han Yan, Liu Xiuming, Chang Liao, Lü Bin, Qu Chen, Guo Xuelian, Yan Junhui, Yan Jun
    Abstract:

    Red Clay underlying the loess-palaeosol sequences on the Chinese Loess Plateau is an Eolian Deposit. There is a controversy over whether magnetic susceptibility (chi) variations in Red Clay sequence can be used as an indicator of summer palaeomonsoon intensity. This study investigates the magnetic mineralogy, magnetic concentration and magnetic grain size distribution of Jiaxian Red Clay with multimagnetic methods. Our results indicate that the magnetic properties of Jiaxian Red Clay are similar to those of the Quaternary loess-palaeosol sequences, and ultrafine ferrimagnetic grains produced during pedogenesis are responsible for an increase in susceptibility, therefore the chi enhancement mechanism of Red Clay is similar to that of the overlying loess-palaeosol sequences. This paper explores chi variations in the Red Clay sequence through spatial and temporal analysis. The susceptibility variation of six sites along a NNE to SSW transect correlate to palaeoclimatic cycles, so chi can be used to trace the summer palaeomonsoon intensity from a spatial perspective. However, a simple loess-derived calibration function cannot be used to quantitative reconstruct the palaeomonsoon intensity variations thought time. An adjusted calibration function for palaeosols from Red Clay sequence needs to be developed, so that chi can be used to quantitative reconstruct palaeomonsoon intensity. Further study is necessary to develop such a transfer function.National Natural Science Foundation of China [41210002, 41202129, 41402149, 41402155, 41501051]; Xinyang Normal University Fund [0201306, 2015GGJS-01]; Nanhu Scholars Program for Young Scholars of XYNUSCI(E)EIARTICLEhanyandili@163.com; xliu@fjnu.edu.cn31421-142920

Zhao Guoyong - One of the best experts on this subject based on the ideXlab platform.

  • Can the magnetic susceptibility record of Chinese Red Clay sequence be used for palaeomonsoon reconstructions?
    'Oxford University Press (OUP)', 2016
    Co-Authors: Zhao Guoyong, Han Yan, Liu Xiuming, Chang Liao, Lü Bin, Qu Chen, Guo Xuelian, Yan Junhui, Yan Jun
    Abstract:

    Red Clay underlying the loess-palaeosol sequences on the Chinese Loess Plateau is an Eolian Deposit. There is a controversy over whether magnetic susceptibility (χ) variations in Red Clay sequence can be used as an indicator of summer palaeomonsoon intensity. This study investigates the magnetic mineralogy, magnetic concentration and magnetic grain size distribution of Jiaxian Red Clay with multimagnetic methods. Our results indicate that the magnetic properties of Jiaxian Red Clay are similar to those of the Quaternary loess-palaeosol sequences, and ultrafine ferrimagnetic grains produced during pedogenesis are responsible for an increase in susceptibility, therefore the χ enhancement mechanism of Red Clay is similar to that of the overlying loess-palaeosol sequences. This paper explores χ variations in the Red Clay sequence through spatial and temporal analysis. The susceptibility variation of six sites along a NNE to SSW transect correlate to palaeoclimatic cycles, so χ can be used to trace the summer palaeomonsoon intensity from a spatial perspective. However, a simple loess-derived calibration function cannot be used to quantitative reconstruct the palaeomonsoon intensity variations thought time. An adjusted calibration function for palaeosols from Red Clay sequence needs to be developed, so that χ can be used to quantitative reconstruct palaeomonsoon intensity. Further study is necessary to develop such a transfer function.9 page(s

  • Can the magnetic susceptibility record of Chinese Red Clay sequence be used for palaeomonsoon reconstructions?
    GEOPHYSICAL JOURNAL INTERNATIONAL, 2016
    Co-Authors: Zhao Guoyong, Han Yan, Liu Xiuming, Chang Liao, Lü Bin, Qu Chen, Guo Xuelian, Yan Junhui, Yan Jun
    Abstract:

    Red Clay underlying the loess-palaeosol sequences on the Chinese Loess Plateau is an Eolian Deposit. There is a controversy over whether magnetic susceptibility (chi) variations in Red Clay sequence can be used as an indicator of summer palaeomonsoon intensity. This study investigates the magnetic mineralogy, magnetic concentration and magnetic grain size distribution of Jiaxian Red Clay with multimagnetic methods. Our results indicate that the magnetic properties of Jiaxian Red Clay are similar to those of the Quaternary loess-palaeosol sequences, and ultrafine ferrimagnetic grains produced during pedogenesis are responsible for an increase in susceptibility, therefore the chi enhancement mechanism of Red Clay is similar to that of the overlying loess-palaeosol sequences. This paper explores chi variations in the Red Clay sequence through spatial and temporal analysis. The susceptibility variation of six sites along a NNE to SSW transect correlate to palaeoclimatic cycles, so chi can be used to trace the summer palaeomonsoon intensity from a spatial perspective. However, a simple loess-derived calibration function cannot be used to quantitative reconstruct the palaeomonsoon intensity variations thought time. An adjusted calibration function for palaeosols from Red Clay sequence needs to be developed, so that chi can be used to quantitative reconstruct palaeomonsoon intensity. Further study is necessary to develop such a transfer function.National Natural Science Foundation of China [41210002, 41202129, 41402149, 41402155, 41501051]; Xinyang Normal University Fund [0201306, 2015GGJS-01]; Nanhu Scholars Program for Young Scholars of XYNUSCI(E)EIARTICLEhanyandili@163.com; xliu@fjnu.edu.cn31421-142920

Qu Chen - One of the best experts on this subject based on the ideXlab platform.

  • Can the magnetic susceptibility record of Chinese Red Clay sequence be used for palaeomonsoon reconstructions?
    'Oxford University Press (OUP)', 2016
    Co-Authors: Zhao Guoyong, Han Yan, Liu Xiuming, Chang Liao, Lü Bin, Qu Chen, Guo Xuelian, Yan Junhui, Yan Jun
    Abstract:

    Red Clay underlying the loess-palaeosol sequences on the Chinese Loess Plateau is an Eolian Deposit. There is a controversy over whether magnetic susceptibility (χ) variations in Red Clay sequence can be used as an indicator of summer palaeomonsoon intensity. This study investigates the magnetic mineralogy, magnetic concentration and magnetic grain size distribution of Jiaxian Red Clay with multimagnetic methods. Our results indicate that the magnetic properties of Jiaxian Red Clay are similar to those of the Quaternary loess-palaeosol sequences, and ultrafine ferrimagnetic grains produced during pedogenesis are responsible for an increase in susceptibility, therefore the χ enhancement mechanism of Red Clay is similar to that of the overlying loess-palaeosol sequences. This paper explores χ variations in the Red Clay sequence through spatial and temporal analysis. The susceptibility variation of six sites along a NNE to SSW transect correlate to palaeoclimatic cycles, so χ can be used to trace the summer palaeomonsoon intensity from a spatial perspective. However, a simple loess-derived calibration function cannot be used to quantitative reconstruct the palaeomonsoon intensity variations thought time. An adjusted calibration function for palaeosols from Red Clay sequence needs to be developed, so that χ can be used to quantitative reconstruct palaeomonsoon intensity. Further study is necessary to develop such a transfer function.9 page(s

  • Can the magnetic susceptibility record of Chinese Red Clay sequence be used for palaeomonsoon reconstructions?
    GEOPHYSICAL JOURNAL INTERNATIONAL, 2016
    Co-Authors: Zhao Guoyong, Han Yan, Liu Xiuming, Chang Liao, Lü Bin, Qu Chen, Guo Xuelian, Yan Junhui, Yan Jun
    Abstract:

    Red Clay underlying the loess-palaeosol sequences on the Chinese Loess Plateau is an Eolian Deposit. There is a controversy over whether magnetic susceptibility (chi) variations in Red Clay sequence can be used as an indicator of summer palaeomonsoon intensity. This study investigates the magnetic mineralogy, magnetic concentration and magnetic grain size distribution of Jiaxian Red Clay with multimagnetic methods. Our results indicate that the magnetic properties of Jiaxian Red Clay are similar to those of the Quaternary loess-palaeosol sequences, and ultrafine ferrimagnetic grains produced during pedogenesis are responsible for an increase in susceptibility, therefore the chi enhancement mechanism of Red Clay is similar to that of the overlying loess-palaeosol sequences. This paper explores chi variations in the Red Clay sequence through spatial and temporal analysis. The susceptibility variation of six sites along a NNE to SSW transect correlate to palaeoclimatic cycles, so chi can be used to trace the summer palaeomonsoon intensity from a spatial perspective. However, a simple loess-derived calibration function cannot be used to quantitative reconstruct the palaeomonsoon intensity variations thought time. An adjusted calibration function for palaeosols from Red Clay sequence needs to be developed, so that chi can be used to quantitative reconstruct palaeomonsoon intensity. Further study is necessary to develop such a transfer function.National Natural Science Foundation of China [41210002, 41202129, 41402149, 41402155, 41501051]; Xinyang Normal University Fund [0201306, 2015GGJS-01]; Nanhu Scholars Program for Young Scholars of XYNUSCI(E)EIARTICLEhanyandili@163.com; xliu@fjnu.edu.cn31421-142920

Han Yan - One of the best experts on this subject based on the ideXlab platform.

  • Can the magnetic susceptibility record of Chinese Red Clay sequence be used for palaeomonsoon reconstructions?
    'Oxford University Press (OUP)', 2016
    Co-Authors: Zhao Guoyong, Han Yan, Liu Xiuming, Chang Liao, Lü Bin, Qu Chen, Guo Xuelian, Yan Junhui, Yan Jun
    Abstract:

    Red Clay underlying the loess-palaeosol sequences on the Chinese Loess Plateau is an Eolian Deposit. There is a controversy over whether magnetic susceptibility (χ) variations in Red Clay sequence can be used as an indicator of summer palaeomonsoon intensity. This study investigates the magnetic mineralogy, magnetic concentration and magnetic grain size distribution of Jiaxian Red Clay with multimagnetic methods. Our results indicate that the magnetic properties of Jiaxian Red Clay are similar to those of the Quaternary loess-palaeosol sequences, and ultrafine ferrimagnetic grains produced during pedogenesis are responsible for an increase in susceptibility, therefore the χ enhancement mechanism of Red Clay is similar to that of the overlying loess-palaeosol sequences. This paper explores χ variations in the Red Clay sequence through spatial and temporal analysis. The susceptibility variation of six sites along a NNE to SSW transect correlate to palaeoclimatic cycles, so χ can be used to trace the summer palaeomonsoon intensity from a spatial perspective. However, a simple loess-derived calibration function cannot be used to quantitative reconstruct the palaeomonsoon intensity variations thought time. An adjusted calibration function for palaeosols from Red Clay sequence needs to be developed, so that χ can be used to quantitative reconstruct palaeomonsoon intensity. Further study is necessary to develop such a transfer function.9 page(s

  • Can the magnetic susceptibility record of Chinese Red Clay sequence be used for palaeomonsoon reconstructions?
    GEOPHYSICAL JOURNAL INTERNATIONAL, 2016
    Co-Authors: Zhao Guoyong, Han Yan, Liu Xiuming, Chang Liao, Lü Bin, Qu Chen, Guo Xuelian, Yan Junhui, Yan Jun
    Abstract:

    Red Clay underlying the loess-palaeosol sequences on the Chinese Loess Plateau is an Eolian Deposit. There is a controversy over whether magnetic susceptibility (chi) variations in Red Clay sequence can be used as an indicator of summer palaeomonsoon intensity. This study investigates the magnetic mineralogy, magnetic concentration and magnetic grain size distribution of Jiaxian Red Clay with multimagnetic methods. Our results indicate that the magnetic properties of Jiaxian Red Clay are similar to those of the Quaternary loess-palaeosol sequences, and ultrafine ferrimagnetic grains produced during pedogenesis are responsible for an increase in susceptibility, therefore the chi enhancement mechanism of Red Clay is similar to that of the overlying loess-palaeosol sequences. This paper explores chi variations in the Red Clay sequence through spatial and temporal analysis. The susceptibility variation of six sites along a NNE to SSW transect correlate to palaeoclimatic cycles, so chi can be used to trace the summer palaeomonsoon intensity from a spatial perspective. However, a simple loess-derived calibration function cannot be used to quantitative reconstruct the palaeomonsoon intensity variations thought time. An adjusted calibration function for palaeosols from Red Clay sequence needs to be developed, so that chi can be used to quantitative reconstruct palaeomonsoon intensity. Further study is necessary to develop such a transfer function.National Natural Science Foundation of China [41210002, 41202129, 41402149, 41402155, 41501051]; Xinyang Normal University Fund [0201306, 2015GGJS-01]; Nanhu Scholars Program for Young Scholars of XYNUSCI(E)EIARTICLEhanyandili@163.com; xliu@fjnu.edu.cn31421-142920

Liu Xiuming - One of the best experts on this subject based on the ideXlab platform.

  • Can the magnetic susceptibility record of Chinese Red Clay sequence be used for palaeomonsoon reconstructions?
    'Oxford University Press (OUP)', 2016
    Co-Authors: Zhao Guoyong, Han Yan, Liu Xiuming, Chang Liao, Lü Bin, Qu Chen, Guo Xuelian, Yan Junhui, Yan Jun
    Abstract:

    Red Clay underlying the loess-palaeosol sequences on the Chinese Loess Plateau is an Eolian Deposit. There is a controversy over whether magnetic susceptibility (χ) variations in Red Clay sequence can be used as an indicator of summer palaeomonsoon intensity. This study investigates the magnetic mineralogy, magnetic concentration and magnetic grain size distribution of Jiaxian Red Clay with multimagnetic methods. Our results indicate that the magnetic properties of Jiaxian Red Clay are similar to those of the Quaternary loess-palaeosol sequences, and ultrafine ferrimagnetic grains produced during pedogenesis are responsible for an increase in susceptibility, therefore the χ enhancement mechanism of Red Clay is similar to that of the overlying loess-palaeosol sequences. This paper explores χ variations in the Red Clay sequence through spatial and temporal analysis. The susceptibility variation of six sites along a NNE to SSW transect correlate to palaeoclimatic cycles, so χ can be used to trace the summer palaeomonsoon intensity from a spatial perspective. However, a simple loess-derived calibration function cannot be used to quantitative reconstruct the palaeomonsoon intensity variations thought time. An adjusted calibration function for palaeosols from Red Clay sequence needs to be developed, so that χ can be used to quantitative reconstruct palaeomonsoon intensity. Further study is necessary to develop such a transfer function.9 page(s

  • Can the magnetic susceptibility record of Chinese Red Clay sequence be used for palaeomonsoon reconstructions?
    GEOPHYSICAL JOURNAL INTERNATIONAL, 2016
    Co-Authors: Zhao Guoyong, Han Yan, Liu Xiuming, Chang Liao, Lü Bin, Qu Chen, Guo Xuelian, Yan Junhui, Yan Jun
    Abstract:

    Red Clay underlying the loess-palaeosol sequences on the Chinese Loess Plateau is an Eolian Deposit. There is a controversy over whether magnetic susceptibility (chi) variations in Red Clay sequence can be used as an indicator of summer palaeomonsoon intensity. This study investigates the magnetic mineralogy, magnetic concentration and magnetic grain size distribution of Jiaxian Red Clay with multimagnetic methods. Our results indicate that the magnetic properties of Jiaxian Red Clay are similar to those of the Quaternary loess-palaeosol sequences, and ultrafine ferrimagnetic grains produced during pedogenesis are responsible for an increase in susceptibility, therefore the chi enhancement mechanism of Red Clay is similar to that of the overlying loess-palaeosol sequences. This paper explores chi variations in the Red Clay sequence through spatial and temporal analysis. The susceptibility variation of six sites along a NNE to SSW transect correlate to palaeoclimatic cycles, so chi can be used to trace the summer palaeomonsoon intensity from a spatial perspective. However, a simple loess-derived calibration function cannot be used to quantitative reconstruct the palaeomonsoon intensity variations thought time. An adjusted calibration function for palaeosols from Red Clay sequence needs to be developed, so that chi can be used to quantitative reconstruct palaeomonsoon intensity. Further study is necessary to develop such a transfer function.National Natural Science Foundation of China [41210002, 41202129, 41402149, 41402155, 41501051]; Xinyang Normal University Fund [0201306, 2015GGJS-01]; Nanhu Scholars Program for Young Scholars of XYNUSCI(E)EIARTICLEhanyandili@163.com; xliu@fjnu.edu.cn31421-142920