哈尔滨黄山黄土粒度特征及其对成因的指示

魏传义; 李长安; 康春国; 常国瑞

doi:10.3799/dqkx.2015.175

Volume 40 Issue 12

Dec. 2015

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Wei Chuanyi, Li Chang'an, Kang Chunguo, Chang Guorui, 2015. Grain-Size Characteristics and Genesis of the Huangshan Loess in Songnen Plain Area. Earth Science, 40(12): 1945-1954. doi: 10.3799/dqkx.2015.175

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Wei Chuanyi, Li Chang'an, Kang Chunguo, Chang Guorui, 2015. Grain-Size Characteristics and Genesis of the Huangshan Loess in Songnen Plain Area. Earth Science, 40(12): 1945-1954. doi: 10.3799/dqkx.2015.175

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Grain-Size Characteristics and Genesis of the Huangshan Loess in Songnen Plain Area

doi: 10.3799/dqkx.2015.175

1.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
State Key Laboratory of Biogeology and Environmental Geology, Wuhan 430074, China
3.
School of Science, Harbin University, Harbin 150086, China

Received Date: 2015-06-05
Publish Date: 2015-12-15

Abstract

Abstract

Huangshan Loess makes a typical example of Northeast China's loess deposition, studying its genesis is the key to reconstruction of both paleoclimate and paleoenvironment of Northeast China. A high resolution and systematic grain size analysis is carried out on "Huangshan Loess" in Harbin area, and the origin of "Huangshan Loess" is discussed in this paper in comparison with many other types of sediment including the modern dust deposition in Harbin area, the loess-palaeosol distributed over the Loess Plateau, the fluvial sediment and Qidingshan Loess in Dalian. The results show that: the 10-50 μm partial group is the "dominant group" of the "Huangshan Loess" whereas the content of < 5 μm partials occupies 23.40%, which is more than the average content of > 50 μm and 5-10 μm particals, corresponding with the composition characteristic of typical eolian loess; The grain-size frequency distribution presents even-number peak and each of these features of grain size parameters are characterized by the atmospheric dust, the average of the σ, SK, KG, Kd, Mz, Md is 1.83, 0.21, 0.86, 2.01, 6.25φ, 5.89φ, respectively; Clay-silt-sand triangular plots of "Huangshan Loess" indicate that it belongs to clayey silt. C-M, L-M, A-M charts and statistical indices of grain size distribution share similarities with various aeolian sediments while obviously differ from fluvial sediments. No one discriminant analysis results is of positive value, which confirms that the "Huangshan Loess" is of the atmospheric sediment just like the aeolian origin of the loess-palaeosol in the Chinese plateau.
- Songnen Plain area,
- Huangshan Loess,
- grain size features,
- eolian origin,
- sediments

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References(86)

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沈阳化工大学材料科学与工程学院沈阳 110142

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Grain-Size Characteristics and Genesis of the Huangshan Loess in Songnen Plain Area

doi: 10.3799/dqkx.2015.175

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