| 从地质现象看成因——浅析哈尔滨地区岗阜状平原上部粉质粘土的成因 |
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| 引用本文： | 林树杰,于飞.从地质现象看成因——浅析哈尔滨地区岗阜状平原上部粉质粘土的成因[J].价值工程,2011,30(6):41-42. |
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| 作者姓名： | 林树杰 于飞 |
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| 作者单位： | 哈尔滨市勘察测绘研究院,哈尔滨,150010 |
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| 摘 要： | 本文通过作者10余年的工作经验及所学的专业知识,从岗阜状平原上部粉质粘土成粉分析、沉积环境、外部应力及物质来原重点阐明了岗阜状平原上部粉质粘土的成因类型。
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| 关 键 词： | 西风带 沉积要素 山岳冰川 沙地 |
To See the Causes from Geological Phenomena:Brief Analysis on Causes of Topping Silty Clay on Gangfuzhuang Plain of Harbin |
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| Lin Shujie,Yu Fei.To See the Causes from Geological Phenomena:Brief Analysis on Causes of Topping Silty Clay on Gangfuzhuang Plain of Harbin[J].Value Engineering,2011,30(6):41-42. |
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| Authors: | Lin Shujie Yu Fei |
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| Institution: | Lin Shujie,Yu Fei(Harbin Survey & Mapping Research Institute,Harbin 150010,China) |
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| Abstract: | In this paper,combined with more than 10 years experience and expertise,the author focuses on genetic type of topping silty clay on Gangfuzhuang plain from silty clay powder generation analysis,sedimentary environment,the external stress and substance. |
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| Keywords: | westerly belt deposition elements mountain glaciers sandy |
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