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泛亚铁路滇西大理至瑞丽沿线主要活动断裂与地震地质特征

吴中海 赵希涛 范桃园 叶培盛 仝亚博 杨振宇

地质通报2012,Vol.31Issue(2):191-217,27.
地质通报2012,Vol.31Issue(2):191-217,27.

泛亚铁路滇西大理至瑞丽沿线主要活动断裂与地震地质特征

Active faults and seismologic characteristics along the Dali-Ruili railway in western Yunnan Province

吴中海 1赵希涛 1范桃园 2叶培盛 1仝亚博 1杨振宇1

作者信息

  • 1. 中国地质科学院地质力学研究所,北京100081
  • 2. 中国科学院地质与地球物理研究所,北京100029
  • 折叠

摘要

Abstract

The new results obtained in active fault survey show that active structure mainly consists of the Zhongdian-Dali-Ruili arcuate fault zone and active western Yunnan block around the Dali-Ruili railway in western Yunnan Province. In the active deformation area, there are ten active faults which prominently influence the crustal stability and earthquake hazard around the area along the Dali-Ruili railway. These active faults are the east piedmont fault of the Diancang Mountain, the Yunlong-Yongping fault zone, the Baoshan fault zone, the Pupiao-Shidian fault, the Taiping-Luomingba fault, the Zhen'an fault zone, the Longxin conjugated fault system, the Huanglianhe conjugated fault system, the Longchuan River fault and the Wanding fault zone from northeast to southwest. Geological and geomorphic evidence for active faulting shows that the activity of the east piedmont fault of the Diancang Mountain, the Baoshan fault zone, the Pupiao-Shidian fault, and the Wanding fault zone were evidently more stronger than other active faults during late Quaternary. Based on the historic and instrumental earthquake data and study results of active faults, the authors drew anew seismic intensity map for the area of the Dali-Ruili railway. The new earthquake intensity map shows that there are at least five high seismic intensity (intensity ^ K) areas along the Dali-Ruili railway. These areas include Dali-Midu, Baoshan, Pupiao-Shidian, Zhen'an-Jingzhuping and Wanding-Ruili from northeast to southwest

关键词

云南大瑞铁路/活动断裂/地震地质/地震烈度分区/地壳稳定性评价

Key words

Dali-Ruili railway/ active faults/ seismology/ seismic intensity/ crustal stability

分类

天文与地球科学

引用本文复制引用

吴中海,赵希涛,范桃园,叶培盛,仝亚博,杨振宇..泛亚铁路滇西大理至瑞丽沿线主要活动断裂与地震地质特征[J].地质通报,2012,31(2):191-217,27.

基金项目

中国地质调查局地质调查项目《泛亚铁路大理至瑞丽沿线地质构造综合研究》(编号:1212010814054)、《云南1∶5万马厂幅、道街坝幅区域地质调查》(编号:1212010784004)、《西南地区活动构造域应力场模拟》(编号:1212010911049)、《青藏高原东南缘重要活动断裂厘定与活动构造体系综合研究》(编号:1212011120163)和基本科研业务费项目《成果集成与战略研究》(编号:DZLXJK201113) (编号:1212010814054)

地质通报

OA北大核心CSCDCSTPCD

1671-2552

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