| 毛乌素沙地沉积物粒度特征与土地沙漠化 |
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| 引用本文： | 李智佩,岳乐平,薛祥煦,杨利荣,王岷,聂浩刚,王飞跃,孙虎.毛乌素沙地沉积物粒度特征与土地沙漠化[J].吉林大学学报(地球科学版),2007,37(3):578-586. |
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| 作者姓名： | 李智佩 岳乐平 薛祥煦 杨利荣 王岷 聂浩刚 王飞跃 孙虎 |
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| 作者单位： | 1．中国地质调查局 西安地质矿产研究所,西安 710054;2．西北大学 大陆动力学国家重点实验室,西安 710069;3．中煤航测遥感应用研究院，西安 710054;4．陕西师范大学 旅游与环境学院，西安 710062 |
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| 基金项目： | 国土资源部国土资源大调查综合研究项目
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陕西省教育厅资助项目
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大陆动力学国家重点实验室资助项目
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西北大学校科研和教改项目 |
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| 摘 要： | 为了研究毛乌素沙地沉积物的粒度特征与土地沙漠化的地质成因类型，通过系统研究沙地及相邻地区晚更新世以来在沙地内部、覆沙黄土区、黄土高原和河流谷地与湖泊等不同地质构造地貌条件下所形成的沉积物粒度特征，指出不同地质成因类型的沉积物是这些地区土地沙漠化的物质基础，区分不同类型的沉积物也是构成不同地质成因类型土地沙漠化分类的理论基础，探讨了不同地质作用对土地沙漠化的贡献及其对土地沙漠化防治方面的意义。研究表明，研究区的土地沙漠化是以各种类型的就地起沙为主要特征，地表径流的水力搬运是沙漠化物质搬运的重要途径。现代毛乌素沙地及其邻区的土地沙漠化是对地质历史时期形成的各种沉积物的进一步搬运、分选和再沉积过程，具有相对复杂的粒度特征。
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| 关 键 词： | 毛乌素沙地 沉积物 粒度特征 土地沙漠化 |
| 文章编号： | 1671-5888（2007）03-0578-09 |
| 收稿时间： | 2006-07-09 |
| 修稿时间： | 2006-07-09 |
Grain-size Distribution Characteristics of Different Geo-Genetic Type Sediments and Land Desertification in Mo Us Desert |
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| LI Zhi-pei,YUE Le-ping,XUE Xiang-xu,YANG Li-rong,WANG Min,NIE Hao-gang,WANG Fei-yue,SUN Hu.Grain-size Distribution Characteristics of Different Geo-Genetic Type Sediments and Land Desertification in Mo Us Desert[J].Journal of Jilin Unviersity:Earth Science Edition,2007,37(3):578-586. |
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| Authors: | LI Zhi-pei YUE Le-ping XUE Xiang-xu YANG Li-rong WANG Min NIE Hao-gang WANG Fei-yue SUN Hu |
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| Institution: | 1．Xi’an Institute of Geological and Mineral Resources，Xi’an 710054,China;2．State Key Laboratory of Continental Dynamics，Northwest University，Xi’an 710069,China;3．Aerial Photogrammetry and Remote Sensing Reconnaissance Institute，Meihang(Group) Industry Development Limited， Xi’an 710054，China;4．College of Tourism and Environmental Science，Shaanxi Normal University, Xi’an 710062，China |
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| Abstract: | In order to explore the grain-size distribution characteristics and geo-genetic types of land desertification in Mo Us desert,the research on the grain-size characteristics of sediments since late Pleistocene has been carried out in the desert area and neighboring area such as inside desert,sand co-vered loess plateau,loess plateau and river valley.The research result shows that sediments of different geologic genetic types are the fundamental material source of sandy desertification in these areas and the distinguishing of different types of the sediments is the theoretical basis of classification of different geo-genetic type of sandy desertification.The contribution of different geological roles on the land desertification and its significance to prevent and deal with the land desertification have also discussed.It is believed that the land desertification in Mo Us desert area is charactrized by the in-situ sand source and the hydraulic carriage by surface flow is the important way to transport the sand.Modern sandy desertification in Mo Us desert and its neighboring regions is a further process of transition,sorting and sedimentation by wind with more intricate grain size distribution characteristics. |
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| Keywords: | Mo Us desert sediment grain size characteristics sandy desertification |
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