威宁现代构造运动触发滑坡的地质背景及数理探讨  

THE GEOLOGICAL BACKGROUND AND MATHEMATICAL PROBE OF THE LANDSLIDE CAUSED BY PRESENT TECTONIC MOVEMENT IN WEINING AREA OF GUIZHOU PROVINCE

作　　者：雷国良[1] 田勇[1] 戎军[2] 

机构地区：[1]贵州科学院,贵阳550001 [2]中国科学院地球化学研究所,贵阳550002

出　　处：《贵州科学》1991年第3期198-203,共6页Guizhou Science

摘　　要：威宁范家岩滑坡系现代构造动运触发。本文简述滑坡的地质背景,对滑坡的机制进行数理探讨:并简评滑坡堆积体的稳定平衡系数对矿区开发运输的影响。Fanjiayan landslide in Weining area was triggered by present tectonic movement,In this paper,we have briefly introduced the landslide geological background and explored mathematically the landslide mechanism.Finally,we also have evaluated the influence of the stable equilibrium coefficient of landslide accumulation on the exploitation and transportation in the mining area nearby.

关 键 词：现代构造运动 滑坡 数理探讨 

分 类 号：P642.22[天文地球—工程地质学]