Results 211 to 220 of about 43,207 (246)
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A Landslide Case Along a Loess Plateau
2013 Fourth International Conference on Digital Manufacturing & Automation, 2013The purpose of this paper is to present a landslide case along a high loess plateau by field investigation, laboratory tests and numerical analysis. The factors of the high loess slope terrain and environmental that induced the landslide are investigated.
Ma Zongyuan, Liao Hongjian, Dang Faning
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Etude de quelques loess du plateau lyonnais
Revue de géographie de Lyon, 1953Pelletier Marcel,Mazenot Georges. Etude de quelques loess du plateau lyonnais. In: Revue de géographie de Lyon, vol. 28, n°4, 1953. pp. 371-375.
Pelletier, Marcel, Mazenot, Georges
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Three-stage collapsibility evolution of Malan loess in the Loess Plateau
CATENA, 2022Hui Yang +4 more
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Loess landscapes of Europe – Mapping, geomorphology, and zonal differentiation
Earth-Science Reviews, 2021Frank Lehmkuhl +2 more
exaly
Types and characteristics of loess landslides at Heifangtai Loess Plateau, China
201020世紀60年代末期,為了安置劉家峽、鹽鍋峽庫區移民,在黑方臺建成了提水灌溉工程,造成地下水位上升,誘發了大量黃土滑坡。作者于2006-04～2007-09先后對黑方臺黃土滑坡進行了野外調查。利用IKONOS影像對黃土滑坡進行了遙感解譯,將其與研究區數字高程模型(DEM)進行疊加再現了滑坡場景。基于以上工作,首先對黑方臺黃土滑坡進行了較為系統的分類,包括黃土泥流、黃土滑動、黃土-泥巖接觸面滑坡、黃土-泥巖順層滑坡和黃土-泥巖切層滑坡。黃土泥流集中發育于野狐狗北部凹地形處;黃土-泥巖滑坡受基巖傾向控制,分布于坡向150°～200°的塬邊地段。農業灌溉補給地下水的增濕、軟化作用是黑方臺黃土滑坡的根本誘發原因。對黑方臺黃土滑坡機制的研究進行了展望。
Dai, F, Kwong, AKL, Min, H, Xu, L
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Genesis and Evolution Mechanism of Loess Tunnels in the Loess Plateau of China
CATENA, 2023Li Wang +4 more
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Distribution and fate of Tibetan Plateau loess
CATENA, 2023Xiangjun Liu +7 more
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