地震地质 ›› 2018, Vol. 40 ›› Issue (5): 1140-1148.DOI: 10.3969/j.issn.0253-4967.2018.05.013

• 研究论文 • 上一篇    下一篇

2014年鲁甸MW6.2地震触发滑坡新编目

吴玮莹1,2, 许冲1   

  1. 1 中国地震局地质研究所, 活动构造与火山重点实验室, 北京 100029;
    2 中国地震局地震预测研究所, 北京 100036
  • 收稿日期:2018-01-22 修回日期:2018-05-18 出版日期:2018-10-20 发布日期:2018-11-29
  • 通讯作者: 许冲,男,1982年生,研究员,研究方向为地震滑坡与活动构造,E-mail:xc11111111@126.com
  • 作者简介:吴玮莹,女,1993年出生,2018年于中国地震局地震预测研究所获构造地质学硕士学位,中国地震局地质研究所在读博士研究生,主要从事地震滑坡易发性评价、地震红外热异常研究,电话:18810552656,E-mail:wuweiying512@126.com。
  • 基金资助:
    “十三五”国家重点研发计划项目(2017YFC1501001)和国家自然科学基金(41661144037)共同资助

A NEW INVENTORY OF LANDSLIDES TRIGGERED BY THE 2014 LUDIAN MW6.2 EARTHQUAKE

WU Wei-ying1,2, XU Chong1   

  1. 1 Key Laboratory of Active Tectonics and Volcano, Institute of Geology, China Earthquake Administration, Beijing 100029, China;
    2 Institute of Earthquake Forecasting, China Earthquake Administration, Beijing 100036, China
  • Received:2018-01-22 Revised:2018-05-18 Online:2018-10-20 Published:2018-11-29

摘要: 文中基于地震前后超高分辨率卫星影像,结合野外调查检验,建立了1个新的2014年鲁甸MW6.2地震触发滑坡的编录成果。结果表明该地震至少触发10 559处同震滑坡,总面积为14.975km2,分布在1个约360km2的椭圆形区域内,这些滑坡的总体积估计为1.24×108m3。研究区内的滑坡点密度、面积百分比与体积密度分别为29.6km-2、4.2%与0.35m。与以前的成果相比,文中得到的滑坡分布图更为详细与准确。文中提供的针对鲁甸地震的详细的地震滑坡编录图,是后续的地震滑坡规律分析与评估的重要基础。

关键词: 2014年鲁甸地震, 同震滑坡, 滑坡编目, 滑坡数量, 滑坡面积

Abstract: Large earthquakes in mountainous areas often induce landslides, which always lead to serious disasters. A detailed and accurate inventory of earthquake-triggered landslides is an important basis for scientific research on co-seismic landslides in the future. High quality landslide inventory should cover the whole earthquake area, spanning all scales of co-seismic landslides that can be detected, accurate landslide locations and boundaries, polygon-based description of the true landslide shape, and separate individual landslides from contiguous landslides group. Building the inventory of landslides triggered by earthquake based on the traditional ground survey will take a long time and a large amount of manpower and material resources, while the remote sensing image, by virtue of its comprehensive coverage and economy, can make up for the shortcomings of the former. In this study, a new inventory of landslides triggered by the 2014 Ludian MW6.2 earthquake is presented on the basis of visual interpretation of pre- and post-earthquake satellite images in very high resolution (~0.5m), and verified by selecting filed investigation. Results show the earthquake triggered at least 10559 landslides around the epicenter. Statistics reveals a total horizontal projection area of 14.975km2, an oval distribution area about 360km2 and an estimated total volume of 1.24×108m3. The landslide number density, landslide area percentage, and landslide volume density are 29.6km-2, 4.2%, 0.35m, respectively. Comparing with previous studies, the inventory of landslides triggered by earthquake in this study is much more detailed and accurate in spatial distribution and the boundaries of landslides are more exquisite, which is attributed to the image quality, resolution and coverage of remote sensing we used in this study and strict compliance with cataloging standards of co-seismic landslides inventory during interpretation. This study provides a detailed and complete inventory related to the 2014 Ludian earthquake, which is an important and essential data for subsequent landslide spatial distribution analyses and assessments. In addition, this study also reminds us that when we establish the inventory of landslides triggered by earthquake with satellite images, it is necessary to select better quality and high-resolution remote sensing images and strictly comply with the standard of co-seismic landslides inventory during interpretation, so as to establish a complete and detailed inventory of landslides triggered by earthquake that can be used to seismic geological disaster analysis and quantitative research.

Key words: the 2014 Ludian earthquake, coseismic landslides, landslide inventory, landslide number, landslide area

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