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作 者:李智佩[1] 岳乐平[1] 薛祥煦[1] 杨利荣[1] 王岷[2] 聂浩刚[2] 王飞跃 孙虎[4]
机构地区:[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
出 处:《吉林大学学报(地球科学版)》2007年第3期578-586,共9页Journal of Jilin University:Earth Science Edition
基 金:国土资源部国土资源大调查项目(20011230004);陕西省教育厅专项科研计划项目;大陆动力学国家重点实验室(西北大学)开放基金资助
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。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 covered 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 geogenetic 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.
分 类 号:X43[环境科学与工程—灾害防治]
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