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冰川泥石流
相关语句
  glacier debris flow
     DISTRIBUTION AND CHARACTERISTICS OF GLACIER DEBRIS FLOW ALONG THE DUSHANZI-KORLA HIGHWAY
     独库公路冰川泥石流分布及其特征
短句来源
     CHARACTERISTICS OF GLACIER DEBRIS FLOW DEPOSIT AND MORAINE FABRIC ALONG DUKU HIGHWAY
     天山独库公路冰川泥石流堆积与冰碛石组构特征
短句来源
  glacial debris flow
     DISCOVERY AND ITS GENETIC EVIDENCES OF EARLY CRETACEOUS GLACIAL DEBRIS FLOW IN THE NORTHEAST MARGIN OF ORDOS
     鄂尔多斯东北缘早白垩世冰川泥石流沉积的发现及其成因证据
短句来源
     Process of Accumulation and Characteristics of Glacial Debris Flow Deposits Trangformed by Moraine
     冰碛转化为冰川泥石流堆积过程及其沉积特征
短句来源
     New Achievements of Studies on the Deposits of Moraine and Glacial Debris Flow
     冰碛与冰川泥石流堆积研究的若干新成果
短句来源
     The glacial debris flow of China
     中国冰川泥石流的一些特征
短句来源
     The glacial debris flow mainly distributes in more than ten modernmelting glacier mountain systems which locate at the west of 102°E, am-oung them, the glacial debris flow in maritime area develops extensively,in subcontinental areas takes a second place in developing extendity anddevelops weakest in extracontinental area.
     中国的冰川泥石流主要分布在东经102°以西、现代冰川急剧消退的10多座山系中,其中海洋型冰川区泥石流最发育,亚大陆型冰川区泥石流次之,极大陆型冰川区泥石流最弱。
短句来源
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  “冰川泥石流”译为未确定词的双语例句
     Evaluation of Activity Degree of GlacierDebris Flow Based on Fuzzy Theory
     基于模糊关系理论的冰川泥石流活动性评价方法
短句来源
     CHARACTERISTICS OF GLACIAL MUD-FLOWS IN SOUTH-EASTERN QINGHAI-XIZANG PLATEAU
     西藏高原东南部冰川泥石流的特征
短句来源
     An Analysis of the Harm and Genesis of Glacial Debris Flows Along the China-pakistan Highway from Kashi to Tashikuergan
     中巴公路喀什至塔什库尔干路段冰川泥石流
短句来源
     Debris flow disastars are distributed mainly along the k136—160 sec- tion, i.e.the Kashi-Tashikuergan section of the China-Pakistan highway.
     冰川泥石流集中分布于该段k136—160之间,大小共有7条泥石流沟,源头为积雪或现代冰川,汇集条件优越,落差可至千米以上。
短句来源
     the mineral maturity index, b/ B value and limonite content of glaical debris flow deposits are also higher than those of moraine.
     冰川泥石流堆积粘土矿物中的伊利石含量低于冰碛,但高岭石的含量又高于冰碛;
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  glacial debris flow
The origin and characteristics of the glacial debris flow in the duku highway of Tianshan Mountains, China
      


On the basis of a series of new discoveries of monographic study in recent years, the paper has had new recognitions in the sequences and features of Fental and Luoquan formation, and has proved that their causes are of"formation of the mud - rock flow from the mountain glaciar in a epicontinental rift and facies of debris fallen which were frozen in the off-shore ice float oron its surface", and has proved into the classif ication of their geological ages etc., thus has set them on a wider background of regional...

On the basis of a series of new discoveries of monographic study in recent years, the paper has had new recognitions in the sequences and features of Fental and Luoquan formation, and has proved that their causes are of"formation of the mud - rock flow from the mountain glaciar in a epicontinental rift and facies of debris fallen which were frozen in the off-shore ice float oron its surface", and has proved into the classif ication of their geological ages etc., thus has set them on a wider background of regional geology. According to the analyses of palaeotectonics and palaeogeography, authors have suggested a new contrast plan of Sinian System in the South and the North of China

本文基于近年来在专题研究中的一系列新的发现,对安徽北部地区的凤台组和罗圈组的层序与特征等,做了新的概括,论证了它们的成因,即属于“陆缘裂谷山岳冰川泥石流和近海浮冰落石相建造”,探讨了其地质时代的归属等问题,进而将其置入更广阔的区域地质背景之上,从古构造和古地理的分析中,对南北方震旦系的对比问题,提出了新的方案。

Debris flow disastars are distributed mainly along the k136—160 sec- tion, i.e.the Kashi-Tashikuergan section of the China-Pakistan highway. There, there are seven debris flow gullies, of which, the Aierkuran gully at k152 and No.l on the Gaizi Rivar gully are the most damaging to the highway. Since 1965, debris flows hava been occurring 1-3 times per year, and often buried the road, blocked or destroyed bridges and culverts.

冰川泥石流集中分布于该段k136—160之间,大小共有7条泥石流沟,源头为积雪或现代冰川,汇集条件优越,落差可至千米以上。泥石流暴发的主要原因是,由于堵塞而形成的突发性冰雪消融洪水,固体物质的主要补给来源是由岩崩和沟岸坍塌而形成的松散堆积物,而陡峻的沟床则为泥石流运动提供了方便。

The Dongru Longba, with a drainage area of 23.74 km2, and 80 km from Bomi County, Tibet, is located along the Chengdu-Lasa Highway. There are 2.06 km2 of modern glacier and snow basin. Debris flows induced by ice-snow melt water occurred repeatedly in the 1960s-1970s. The Yupu Zangbu River section of Palong Zangbu River was blocked up and changed to a lake, which destroyed the roadbed of the Chengdu-Lasa Highway.

以积雪融水为主的冰川泥石流通常在夏初爆发,主沟中下游的崩塌、滑坡堵沟是固体物质的重要来源之一。本文记述了一场典型的冰雪融水泥石流过程及危害。讨论了冬茹弄巴冰雪融水泥石流趋势是在减弱,川藏公路通过该沟方案可采取防御中等规模泥石流修建半永久性桥的对策。从分析波密地区水热组合变化得到了预报中长期冰川泥石流发生的一个气候判据。

 
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