Paleoclimatic significance of the temperature dependent susceptibility of halocene loess along a NW SE transeet in the Chinese loess plateau

Geophysical Research Letters

Volumn 27, Issue 22, 2000, Pages 3715-3718

  Deng, Chenglong ^a   Zhu, Rixiang ^a   Verosub, K L ^b   Singer, M J ^b   Yuan, Baoyin ^a  

^a INSTITUTE OF GEOLOGY AND GEOPHYSICS   (China)

^b UNIVERSITY OF CALIFORNIA   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

HOLOCENE; LOESS; MAGNETIC SUSCEPTIBILITY; PALEOCLIMATE;

CHINA; LOESS PLATEAU;

CLIMATE CHANGE; LANDFORMS; MAGNETIC SUSCEPTIBILITY; MAGNETITE; MODEMS; TEMPERATURE DISTRIBUTION; X RAY DIFFRACTION ANALYSIS; ATMOSPHERIC TEMPERATURE; SAND; SEDIMENTS; SILT;

CHINESE LOESS; CHINESE LOESS PLATEAU; CLIMATIC CHANGES; CLIMATIC VARIABLES; PALEOCLIMATIC SIGNIFICANCE; PEDOGENIC PROCESS; TEMPERATURE DEPENDENCE; TEMPERATURE DEPENDENT;

SEDIMENTS; GEOMAGNETISM;

CITRATE BICARBONATE DITHIONITE TREATMENT; HOLOCENE LOESS; MAGHEMITE; TEMPERATURE DEPENDENCE OF SUSCEPTIBILITY;

EID: 0034351930     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/2000GL008462     Document Type: Article

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