首页|贵州碎屑岩分布区崩塌地质灾害发育特征及孕灾条件分析

贵州碎屑岩分布区崩塌地质灾害发育特征及孕灾条件分析

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碎屑岩分布区地质灾害以滑坡为主,而崩塌地质灾害往往容易被忽视.通过对碎屑岩崩塌孕育条件的分析,可以更好地指导碎屑岩分布区崩塌的防治工作.本文以云贵山崩塌为例,运用地面调查、遥感、数值模拟等技术手段,分析其地质灾害特征、运动特征及孕育条件.采用归纳分析的方法对碎屑岩崩塌孕灾条件进行了总结.结论显示,云贵山崩塌为小型崩塌,破坏模式多为倾倒式,影响范围112 m以内;陡峭的地形、硬岩夹软弱夹层组合、近水平斜坡结构、差异性风化是云贵山崩塌的主要孕育条件;碎屑岩崩塌孕灾条件中地形地貌、特殊岩性组合及软硬岩接触面的揭露情况对碎屑岩崩塌孕育的影响较大.
Analysis of development characteristics and inducing conditions of collapses in the distribution area of clastic rocks in Guizhou
Landslide is the main geological hazard in the distribution area of clastic rocks,and collapse is often ig-nored.The analysis of the inducing conditions of clastic rock collapses can guide the prevention and control of col-lapses in the distribution area of clastic rocks.Taking Yungui Mountain Collapse as an example,this paper uses ground survey,remote sensing,numerical simulation and other technical means to analyze its geological disaster characteristics,movement characteristics and inducing conditions.The induction analysis method is used to summa-rize the inducing conditions of clastic rock collapses.The results show that the Yungui Mountain Collapse is a small collapse,the failure mode is mostly tipping,and the influence range is within 112 m.Steep terrain,combination of hard rock and weak interlayers,near-horizontal slope structure and differential weathering are the main inducing conditions of Yungui Mountain Collapse.Geomorphology,special lithology combination and exposure of the contact surface between hard and soft rocks have great influence on the formation of clastic rock collapses.

clastic rockcollapsedifferential weatheringhazard-inducing conditions

段方情、何松标、马骅

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贵州省地质环境监测院,贵州 贵阳 550001

贵州地环工程有限公司,贵州 贵阳 550001

碎屑岩 崩塌 差异风化 孕灾条件

中央资金中央自然灾害防治体系建设项目

Z195110010003

2024

贵州科学
贵州科学院

贵州科学

影响因子:0.395
ISSN:1003-6563
年,卷(期):2024.42(1)
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