冰川泥石流

冰川泥石流是由冰碛物与冰雪融水混合形成的一种碎屑重力流沉积。

Glacial debris flow is a kind of debris gravitational flow deposits that result from the mix of moraines and ice snow melt water .

冰碛与冰川泥石流堆积研究的若干新成果

New Achievements of Studies on the Deposits of Moraine and Glacial Debris Flow

独库公路冰川泥石流分布及其特征

Distribution and characteristics of glacier debris flow along the dushanzi-korla highway

天山独库公路冰川泥石流堆积与冰碛石组构特征

Characteristics of glacier debris flow deposit and moraine fabric along Duku highway

气温控制区内冰川泥石流分布较广，区内泥石流的爆发主要受气温的影响；

In temperature dominating area , glacier debris flows are widely distributed , which are affected by the fluctuating temperature .

最后，使用该方法对该路段某些大型、特大型冰川泥石流灾害的危险性进行了动态分析。

The approach is applied to analyze the dynamic hazard of some large-scale or oversize glacier debris flows in the section .

发现冰川泥石流堆积的基质指数和磨蚀指数均大于冰碛的基质指数和磨蚀指数；

The studies show that the basement index and abrasion index of glacial debris flow deposits are usually higher than those of moraine ;

泥石流以暴雨沟谷型泥石流为主，可见少量暴雨坡面型泥石流及古冰川泥石流。

The main type of debris flow occurs in gulch by rainstorm , a small amount occurs on slope by rainstorm , and some others are coursed by glacial action .

北美东部的一种沼泽兰花，花纯白、流苏状，穗状花序。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

Bog orchid of eastern North America with a spike of pure white fringed flowers . DISCOVERY AND ITS GENETIC EVIDENCES OF EARLY CRETACEOUS GLACIAL DEBRIS FLOW IN THE NORTHEAST MARGIN OF ORDOS

磨西河流域是我国西南典型的强震区和冰川泥石流的集中发育区，且泥石流的发育和发生均表现出了与冰川冰碛、构造运动强度及气候环境相关的响应特征。

Moxi river located in the southwestern of China , where is a concentrative glacial debris flow area . The debris flow represents some characters related to moraine , Intensity of tectonic movement and climate environment .

云南东川末次冰期冰川与泥石流发育的区域性特征

Regional Characteristics of Glacier and Debris Flow Development in Dongchuan , Yunan Province

悼念冰川水文和泥石流学者&王文浚同志

Condolence to Comrade Wang wenjun & scholar in glacial hydrology and debris flow

贡嘎山区全新世冰川变化与泥石流发育的关系

Relationship between the glacier variation and the debris flow development of the Holocene in the Gongga mountainous region

因此为探讨冰川作用、泥石流活动、重力崩塌等过程提供了一种重要的方法和技术途径。

Therefore , it provides an important method to study glacial processes , activities of debris flow and rock collapse etc.

在对庐山地质演变、山顶土壤和几处典型地貌分析的基础上，提出一种猜想：庐山地貌可能是温暖湿润的气候条件下的水成地貌，第四纪既无冰川也无泥石流的发生。

The author bases a guess on the analysis of soil at the mountaintop and several typical landforms at the Lushan mountains : the landforms of Lushan mountains is shaped under the warm and moist climate , or is shaped by water eroding glaciation formed earlier .

分布于高山冰川与积雪边缘、固体物质主要由新老冰碳和雪崩岩屑所补给、水源依赖于冰雪融水及冰湖溃决水的泥石流称为冰川泥石流。

Located in the edge of mountain glaciers and snow cover , solid substances are mainly old and new ice from the debris of the supply of carbon and avalanches , water dependent on snow melt water and glacial lake outburst known as glacial debris debris flow of water .