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滇西大理至瑞丽铁路龙陵段主要的地质灾害类型及其发育规律

熊昌利 陈亮 魏昌利 贾小川 罗明 杨学俊 罗改

地质通报2012,Vol.31Issue(2):396-405,10.
地质通报2012,Vol.31Issue(2):396-405,10.

滇西大理至瑞丽铁路龙陵段主要的地质灾害类型及其发育规律

Main geohazard types in Longling segment of the Dali-Ruili railway, western Yunnan and their development characteristics

熊昌利 1陈亮 2魏昌利 1贾小川 1罗明 1杨学俊 1罗改1

作者信息

  • 1. 四川省地质调查院,四川成都610081
  • 2. 成都理工大学,四川成都610059
  • 折叠

摘要

Abstract

Longling area along the Dali-Ruili railway is located in western Yunnan canyon area of Yunnan Plateau, in the watershed zone between the Nujiang River and the Irrawaddy River drainages, where new tectonic movement is intense and seismic activity occurs frequendy. The rainfall in this area is focus on May~October, and the rainfall intensity is large and concentrated. Because of the complicated geological environment, with the addition of rainfall, human activities and other exterior factors, geohazards such as collapses, landslides and debris flow have repeatedly occurred in this area, which often cause accidents such as washing out paddy fields and forests, destroying highways, bridges and buildings, and personnel casualties. The authors analyzed the distribution, formation conditions and development regularity of main geohazards in this area. The result obtained provides a geological basis for the planning and construction of the Dali-Ruili railway and social economic development of the surveyed zone.

关键词

大理-瑞丽铁路/滇西/地质灾害/发育规律

Key words

Dali-Ruili railway/ western Yunnan Province/ geohazard/ development characteristics

分类

天文与地球科学

引用本文复制引用

熊昌利,陈亮,魏昌利,贾小川,罗明,杨学俊,罗改..滇西大理至瑞丽铁路龙陵段主要的地质灾害类型及其发育规律[J].地质通报,2012,31(2):396-405,10.

基金项目

中国地质调查局项目《云南1∶5万清河街幅、镇安街幅、龙陵县幅、龙新幅区域地质调查》(编号:1212010784006) (编号:1212010784006)

地质通报

OA北大核心CSCDCSTPCD

1671-2552

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