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首页> 外文期刊>Journal of earth system science >Earthquake hazard in northeast India a€“ A seismic microzonation approach with typical case studies from Sikkim Himalaya and Guwahati city
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Earthquake hazard in northeast India a€“ A seismic microzonation approach with typical case studies from Sikkim Himalaya and Guwahati city

机译:印度东北部的地震灾害-地震微区带方法,以锡金喜马拉雅山和古瓦哈提市为例

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摘要

A comprehensive analytical as well as numerical treatment of seismological, geological, geomorphological and geotechnical concepts has been implemented through microzonation projects in the northeast Indian provinces of Sikkim Himalaya and Guwahati city, representing cases of contrasting geological backgrounds a€“ a hilly terrain and a predominantly alluvial basin respectively. The estimated maximum earthquakes in the underlying seismic source zones, demarcated in the broad northeast Indian region, implicates scenario earthquakes of e?‘€e?‘? 8.3 and 8.7 to the respective study regions for deterministic seismic hazard assessments. The microzonation approach as undertaken in the present analyses involves multi-criteria seismic hazard evaluation through thematic integration of contributing factors. The geomorphological themes for Sikkim Himalaya include surface geology, soil cover, slope, rock outcrop and landslide integrated to achieve geological hazard distribution. Seismological themes, namely surface consistent peak ground acceleration and predominant frequency were, thereafter, overlaid on and added with the geological hazard distribution to obtain the seismic hazard microzonation map of the Sikkim Himalaya. On the other hand, the microzonation study of Guwahati city accounts for eight themes a€“ geological and geomorphological, basement or bedrock, landuse, landslide, factor of safety for soil stability, shear wave velocity, predominant frequency, and surface consistent peak ground acceleration. The five broad qualitative hazard classifications a€“ `lowa€?, `moderatea€?, `higha€?, `moderate higha€? and `very higha€? could be applied in both the cases, albeit with different implications to peak ground acceleration variations. These developed hazard maps offer better representation of the local specific seismic hazard variation in the terrain.
机译:印度东北部锡金喜马拉雅和古瓦哈提市的微区划项目已对地震,地质,地貌和岩土工程概念进行了全面的分析和数值处理,代表了地质背景形成对比的案例,例如丘陵地带和主要地带冲积盆地。在印度东北部广泛地区划定的潜在地震震源区中估计的最大地震,意味着情景为“?e?”? 8.3和8.7到各自的研究区域进行确定性的地震危险性评估。本分析中采用的微区划方法涉及通过归纳因素的专题综合评估多准则地震灾害。锡金喜马拉雅山的地貌主题包括地表地质,土壤覆盖,斜坡,岩石露头和滑坡,以实现地质灾害分布。之后,将地震主题(即地面一致的峰值地面加速度和优势频率)叠加并添加到地质灾害分布中,以获得锡金喜马拉雅山的地震灾害微带化图。另一方面,古瓦哈提市的微区研究涉及八个主题:地质和地貌,基底或基岩,土地利用,滑坡,土壤稳定性的安全系数,剪切波速度,主要频率以及地面一致的峰值地面加速度。五个主要的定性危害分类为“低”,“中”,“高”,“中”。和“很高”?尽管对峰值地面加速度变化有不同的影响,但两种情况都可以应用。这些已开发的灾害图可以更好地表示地形中局部特定地震灾害的变化。

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