| 九寨沟诺日朗瀑布钙华震损机制分析 |
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| 引用本文： | 魏良帅,梁波,刘民生,吴森,肖维阳,刘勇.九寨沟诺日朗瀑布钙华震损机制分析[J].沉积与特提斯地质,2022,42(4):675-683. |
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| 作者姓名： | 魏良帅 梁波 刘民生 吴森 肖维阳 刘勇 |
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| 作者单位： | 中国地质科学院探矿工艺研究所, 四川 成都 611734;四川省地质工程勘察院集团有限公司, 四川 成都 610072;九寨沟风景名胜区管理局, 四川 阿坝 623402 |
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| 基金项目： | 中国地质调查局地质调查项目长江上游水文地质与水资源调查监测(DD20221757) |
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| 摘 要： | 2017年8月8日九寨沟发生7.0级地震，景区内部分景观破损，其中诺日朗瀑布钙华体局部出现小规模坍塌。通过调查研究，查明了瀑布景观钙华的震损现状，结合二维离散元分析软件Universal Distinct Element Code (UDEC)对变形破坏过程进行了模拟分析，揭示了钙华震损过程分为振动蠕变、持续拉张、倾倒折断和溃屈破坏4个阶段。综合地质环境背景分析，景观钙华形成的地质环境条件和景区水流系统处于基本稳定状态，景观体处于相对稳定的发展阶段，层湖叠瀑景观不会消亡。
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| 关 键 词： | 九寨沟地震 诺日朗瀑布 钙华震损 机制分析 |
| 收稿时间： | 2021/10/20 0:00:00 |
| 修稿时间： | 2022/6/24 0:00:00 |
Analysis of seismic damage mechanism of travertine at Nuorilang waterfall, Jiuzhaigou |
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| WEI Liangshuai,LIANG Bo,LIU Minsheng,WU Sen,XIAO Weiyang,LIU Yong.Analysis of seismic damage mechanism of travertine at Nuorilang waterfall, Jiuzhaigou[J].Sedimentary Geology and Tethyan Geology,2022,42(4):675-683. |
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| Authors: | WEI Liangshuai LIANG Bo LIU Minsheng WU Sen XIAO Weiyang LIU Yong |
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| Affiliation: | Institute of Exploration Technology CAGS, Chengdu 611734, China;Sichuan Institute of Geological Engineering Investigation Group Co. LTD, Chengdu 610072, China;Jiuzhaigou Valley Scenic and Historic Interest Area administration, Aba Tibetan and Qiang Autonomous Prefecture 623402, China |
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| Abstract: | The Jiuzhaigou earthquake that occurred on August 8, 2017, has caused damage to some landscapes in the scenic area, including a small-scale collapse of the travertine located in the famous Nuorilang waterfall. Based on investigation, the current situation of seismic damage to the travertine has been determined. Besides, the damage process of the travertine has been simulated and analyzed through the two-dimensional discrete element analysis method (Universal Distinct Element Code, UDEC). The process reveals that the travertine has experienced four stages: vibration creep, continuous tension, toppling fracture and buckling failure. According to the analysis of seismic damage process of the travertine and its geological environment background, the geological environment conditions for the formation of travertine and the water flow system in the scenic area are basically stable, so the travertine will be in a relatively stable development stage, and the famous waterfall landscape will not die out. |
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| Keywords: | Jiuzhaigou earthquake Nuorilang waterfall travertine seismic damage process mechanism analysis |
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