新平新化乡滑坡形成机制及地质灾害风险管控措施  

FORMATION MECHANISM OF LANDSLIDE AND RISK CONTROL MEASURES OF GEOLOGICAL HAZARD IN XINHUA TOWNSHIP,XINPING

作　　者：丁中开 张卫锋 杨文礼 DING Zhong-kai;ZHANG Wei-feng;YANG Wen-li(Key Laboratory of Geohazard Forecast and Geoecological Restoration in Plateau Mountainous Area,MNR,Kunming 650216;Key Laboratory of Geohazard Forecast and Geoecological Restoration in Plateau Mountainous Area of Yunnan Province,Kunming 650216;Yunnan Institute of Geological Environment Monitoring,Kunming 650216)

机构地区：[1]自然资源部高原山地地质灾害预报预警与生态保护修复重点实验室,云南昆明650216 [2]云南省高原山地地质灾害预报预警与生态保护修复重点实验室(筹),云南昆明650216 [3]云南省地质环境监测院,云南昆明650216

出　　处：《云南地质》2024年第2期263-268,共6页Yunnan Geology

摘　　要：本文以云南哀牢山区新平县新化集镇滑坡为研究对象,在研究区内孕灾地质背景条件的基础上,分析了滑坡的变形破坏特征及其形成机制,结合岩土体试验,对坡体稳定性进行了评价,提出了合理的地质灾害风险管控措施建议。On the basis of the regional geological background conditions,the deformation and failure characteristics and formation mechanism of the landslides in the Xinhuaji Town,Xinping County,Ailaoshan Areawere analyzed in this study.Combined with the rock and soil test,the slope stability was evaluated,and reasonable geological disaster risk control measures were proposed.

关 键 词：滑坡 地质灾害 形成机制 地质灾害风险管控 新化乡 云南新平 

分 类 号：P642.22[天文地球—工程地质学]