中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
滇东北蒋家沟粘性泥石流堆积地貌

文献类型:期刊论文

作者田连权
刊名山地研究
出版日期1991
卷号9期号:3页码:185-192+205
关键词滇东北 蒋家沟 粘性泥石流 堆积地貌
其他题名ACCUMULATIONAL LANDFORM OF VISCOUS DEBRIS IN JIANG JIA RAVINE, NORTHEAST YUNNAN
通讯作者田连权
中文摘要据成因,把泥石流堆积地貌分为自然堆积地貌和人为堆积地貌。据堆积过程,把自然泥石流堆积地貌分为古泥石流台地、老泥石流台地和近代泥石流长柄扇。据建筑物引起的堆积形态,把人为堆积地貌分为泥石流堆积扇(锥)、回淤泥砾滩、侧积泥砾堤和堰塞洼地。
英文摘要 Based on the field investigations, classification of accumulationsl landforms in Jiangjia Ravine is made in this paper. According to the genesis,the accumulational landform of debris flow may be classified into natural and man-made ones. According to the accumulated processes, the natural accumulational landform may be classified into paleo-platform of debris flow(Q3),old platform of debris flow(Q4)and recent fan with long handle(before 1000 years). The man-made accumulational landforms may be classified into fan of levee tail,fan (cone) of branch gully, mud-gravel beach for bach deposit,mud-gravel dyke for side deposit and barrier depression. The accumulational landforms of debris flow will induce the deposit conditions to changed Therefore, the deposit conditions may be improved due to rational distribution of the construction.
学科主题灾害学
收录类别CSCD
语种中文
CSCD记录号CSCD:153468
公开日期2011-09-09
源URL[http://192.168.143.20:8080/handle/131551/3491]  
专题成都山地灾害与环境研究所_成都山地所知识仓储(2009年以前)
推荐引用方式
GB/T 7714
田连权. 滇东北蒋家沟粘性泥石流堆积地貌[J]. 山地研究,1991,9(3):185-192+205.
APA 田连权.(1991).滇东北蒋家沟粘性泥石流堆积地貌.山地研究,9(3),185-192+205.
MLA 田连权."滇东北蒋家沟粘性泥石流堆积地貌".山地研究 9.3(1991):185-192+205.

入库方式: OAI收割

来源:成都山地灾害与环境研究所

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