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“8·12”山阳滑坡视向滑动特征与运动过程

王佳运 李林 郑定国 武立

灾害学2018,Vol.33Issue(1):111-116,6.
灾害学2018,Vol.33Issue(1):111-116,6.DOI:10.3969/j.issn.1000-811X.2018.01.020

“8·12”山阳滑坡视向滑动特征与运动过程

Characteristics of Apparent Dip Slide and Movement Process of the 8.12 Shanyang Rockslide

王佳运 1李林 2郑定国 2武立1

作者信息

  • 1. 长安大学地质工程与测绘学院,陕西西安710054
  • 2. 国土资源部黄土地质灾害重点实验室/中国地质调查局西安地质调查中心,陕西西安710054
  • 折叠

摘要

Abstract

At 00:30 a.m.August 12th 2015,a rockslide with the volume of 1.68 million cubic meters occurred in Zhongcun town,Shanyang in Shaanxi province,which resulted in a catastrophic rockslide with 8 death,57 persons missing and nearly 0.5 billion RMB direct economic loss.Based on the investigation of geometric dimension,structure of sliding rockmass and the shear outlet,the geological conditions of apparent dip slide of the rockslide were analyzed according to the following factors including Bedding block-broken body,Inclined rockmass barrier,Apparent dip exiting,driving-rock mass sliding and the slide resisting block;and it was considered that the Shanyang rockslide took on typical characteristics of apparent dip slide which included long-term creeping along the dip angle and intercalated sliding in the slide bed,and overall slide with high-locality along the apparent dip angle.By the means of analyzing the movement process and the structure distribution of the sliding mass,the movement process of the rockslide can be divided into apparent dip shear slide zone,main slide accumulation zone,collision and retracing accumulation zone,fragment scattering zone.

关键词

“8·12”山阳滑坡/厚层陡倾斜向结构/视向滑动/运动过程

Key words

8.12 Shanyang rockslide/steep oblique inclined thick bedding structure/apparent dip sliding/movement process

分类

天文与地球科学

引用本文复制引用

王佳运,李林,郑定国,武立..“8·12”山阳滑坡视向滑动特征与运动过程[J].灾害学,2018,33(1):111-116,6.

基金项目

中国地质调查局地质调查项目“吕梁山区城镇地质灾害调查”(121201011000150018) (121201011000150018)

灾害学

OA北大核心CSCDCSTPCD

1000-811X

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