现代地质
現代地質
현대지질
GEOSCIENCE-JOURNAL OF GRADUATE SCHOOL CHINA UNIVERSITY OF GEOSCIENCES
2014年
2期
429-437
,共9页
常宏%韩会卿%章昱%李景富%谭建民
常宏%韓會卿%章昱%李景富%譚建民
상굉%한회경%장욱%리경부%담건민
滑坡%崩塌%成灾模式%清江流域%鄂西
滑坡%崩塌%成災模式%清江流域%鄂西
활파%붕탑%성재모식%청강류역%악서
landslide%avalanche%formation pattern of landslides and avalanches%Qingjiang river basin%west-ern Hubei
鄂西清江流域是我国滑坡崩塌地质灾害易发区。在该区域11个县市地质灾害详细调查成果基础上,运用归纳和类比等方法,对区内2276个滑坡和567个崩塌(危岩)的要素数据进行统计分析;归纳总结了区域滑坡崩塌的基本发育特征和分布规律,并从构造作用、岩性组合、河流地貌演化、人类活动、降雨等几个方面,分析多种致灾背景对滑坡崩塌的不同影响和控制作用;继而根据主控因素归纳分析了区内滑坡具有的降雨型、箱形(紧窄)背斜型、宽缓向斜型和水库型等4类主要成灾模式,以及崩塌(危岩)具有的宽缓向斜型和岩溶石柱型两类主要成灾模式;指出了今后需要重点防控的三种类型滑坡崩塌风险。
鄂西清江流域是我國滑坡崩塌地質災害易髮區。在該區域11箇縣市地質災害詳細調查成果基礎上,運用歸納和類比等方法,對區內2276箇滑坡和567箇崩塌(危巖)的要素數據進行統計分析;歸納總結瞭區域滑坡崩塌的基本髮育特徵和分佈規律,併從構造作用、巖性組閤、河流地貌縯化、人類活動、降雨等幾箇方麵,分析多種緻災揹景對滑坡崩塌的不同影響和控製作用;繼而根據主控因素歸納分析瞭區內滑坡具有的降雨型、箱形(緊窄)揹斜型、寬緩嚮斜型和水庫型等4類主要成災模式,以及崩塌(危巖)具有的寬緩嚮斜型和巖溶石柱型兩類主要成災模式;指齣瞭今後需要重點防控的三種類型滑坡崩塌風險。
악서청강류역시아국활파붕탑지질재해역발구。재해구역11개현시지질재해상세조사성과기출상,운용귀납화류비등방법,대구내2276개활파화567개붕탑(위암)적요소수거진행통계분석;귀납총결료구역활파붕탑적기본발육특정화분포규률,병종구조작용、암성조합、하류지모연화、인류활동、강우등궤개방면,분석다충치재배경대활파붕탑적불동영향화공제작용;계이근거주공인소귀납분석료구내활파구유적강우형、상형(긴착)배사형、관완향사형화수고형등4류주요성재모식,이급붕탑(위암)구유적관완향사형화암용석주형량류주요성재모식;지출료금후수요중점방공적삼충류형활파붕탑풍험。
The mountain area in western Hubei Province,mainly in Qingjing river basin,is one of landslide and avalanche prone regions in China.Based on the results of the geological disaster investigation in 1 1 counties of this area,including 2,276 landslides and 567 avalanches,the characteristics of development and distribution of these landslides and avalanches are summarized in this paper by the method of statistics,induction and analo-gy.At the same time the control effect of different hazard-cause factors was respectively analyzed,including geological structures,lithology combination,river evolution,human activities and rainfalls.According to the key controlling factor,the formation patterns of landslides can be sorted into 4 types of regular ones,i.e.rain-fall controlled type,box-shape (close-narrow shape)anticline controlled type,wide and gentle shape syncline controlled type,and reservoir water-level controlled type,and those of avalanches can be classified into 2 types of regular ones,i.e.wide and gentle shape syncline controlled type,and karst-pillar controlled type.At last it was inferred that the risk of 3 types of landslides and avalanches must be focused on and prevented in the study area.