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diluvial相关的网络例句

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与 diluvial 相关的网络例句 [注:此内容来源于网络,仅供参考]

Along the fault we may recognize at least eight fault scarps or steep fault slopes whose heights are 0.33-0.62 m, 4.3-5.2 m, 6.8-8.3 m, 10-11.8 m,~16 m, 20-28 m, 45-50 m and 65-80 m respectively, as well as river terraces, diluvial fans and spring sinter platforms that may largely correspond with these fault scarps.

沿断层至少可以识别出高度分别为0.33~0.62m、4.3~5.2m、6.8~8.3m、10~11.8m、约16m、20~28m、45~50m和65~80m的8套断层崖或断层陡坎,以及与各级断层崖大致对应的河流阶地、洪积扇和泉华台地。

According to analytical results, the Haihe River Basin is divided into 7 zones: Taihang and Yanshan mountainous zone, piedmont diluvial/alluvial zone, Beijing-Tianjin-Tangshan region, piedmont plain zone, middle and eastern plain zone, Tianjin downtown area, and Tuhai Majia River plain. This result accords with water resources management in the Haihe River Basin.

作者根据环境、粮食、水资源和社会经济4大类30个指标,利用聚类分析方法和地理信息系统等工具,分析其聚类过程,把海河流域分为太行、燕山山区、山前洪、冲积扇区、京津唐地区、山前平原区、中东部平原区和淀东清南天津区和徒骇马颊河平原区7个区,分区结果符合流域水资源管理的要求。

There are seven vegetation belts in Helan Mountain-Yinchuan Basin system from west to east,they are mountain forest belt,mountain shrub-grass belt,mountain foot desert grassland belt,oasis belt in diluvial fan plain,oasis belt in alluvial plain,wetland belt near the Yellow river, desert grassland belt in ordos platform.

基于整个山盆系统内山地、平原、黄河、台地上分布的7个自然植被带,提出了山地-平原绿洲—黄河—台地的生产生态范式。

In view of Helan Mountain-Yinchuan basin is a ecological Continuum, it's innovative to put forward the holistic system of Helan Mountain-Yinchuan Basin as suitable scale for landscape management. Based on the fact that Helan Mountain-Yinchuan Basin in a circle composed by deserts and Loess Plateau,and seven vegetation ( the mountain forest belt,mountain shrub-grass belt,mountain foot desert grassland belt,oasis belt in diluvial fan plain,oasis belt in alluvial plain,wetland belt near the Yellow river, desert grassland belt in Obrdos platform) belong to the system, a"mountain-plain oasis-river-platform eco-productive paradigm"is proposed.

基于贺兰山——银川盆地是一个生态连续的复合系统,创新性地提出以整个山盆系统做为景观整体管理的尺度;基于贺兰山——银川盆地处于生态脆弱圈内山地森林带、山地灌草带、山麓荒漠草原带、洪积平原带、黄河冲积平原带、黄河滩涂湿地带、鄂尔多斯台地荒漠草原带等7个植被带的水平和垂直地带性特点,提出了贺兰山——银川盆地系统山地-平原绿洲—黄河—台地的生产生态范式。

A important conclusion is that fluvial-lacustrine, karst, diluvial, colluvial, glacial and outwash deposits, which formed between early Pleistocene and early middle-Pleistocene, have high cement degree, low permeability, high intensity, low deformation, and good engineering properties, but modern riverbed phase deposits, which formed in between late middle-Pleistocene and Holocene, are loose, highly permeable, weak, highly deformable and have bad engineer characteristics, so they are susceptive to differential settlement, piping, drafting, liquefaction problems.

得出早更新世—中更新世早期河湖相沉积、岩溶沉积、洪积、崩坡积、冰碛和冰水沉积密实度高,胶结较好,透水性差,强度高,变形小,工程性质较好,而中更新世晚期—全新世现代河床沉积较松散,渗透性高,强度较低,变形较大,易发生差异沉降、管涌、流土、地震液化等工程地质问题的重要结论。

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