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首页> 外文期刊>International Journal of Computer Trends and Technology >Data Mining Techniques for Earthquake Frequency-Magnitude Analysis and Seismic Zone Estimation
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Data Mining Techniques for Earthquake Frequency-Magnitude Analysis and Seismic Zone Estimation

机译:地震频响分析和地震带估计的数据挖掘技术

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摘要

India has had a number of the world's greatest earthquakes in the last century. In fact, more than 50% area in the country is considered prone to damaging earthquakes. The northeastern region of the country as well as the entire Himalayan belt is susceptible to great earthquakes of magnitude more than 8.0. The main cause of earthquakes in these regions is due to the movement of the Indian plate towards the Eurasian plate at the rate of about 50 mm per year. The earthquake zoning map of India divides India into 4 seismic zones (Zone 2, 3, 4 and 5). According to the present zoning map, Zone 5 expects the highest level of seismicity whereas Zone 2 is associated with the lowest level of seismicity. In this Paper, we have derived regression relations on Earthquake Magnitudefrequency Data Set using statistical tools like SAS (Statistical Analysis System) and Weka (Waikato Environment for Knowledge Analysis). The regression relations obtained are the first relations for this region. In Earthquake Disaster Management Data Set, Magnitude is considered as a Dependent variable. It depends on LocationRank, StateRank, Elevation, Population, Year, Month, Day, Hour, Minute, Sec, Latitude, Longitude and Depth which are considered as Independent Variables. Based on Dependent and Independent variables, the new ‘seismic zone’ can be analyzed at different earthquake locations. If magnitude is equal to 7 or more, large areas are damaged depending on their depth. If magnitude is equal to 3 or less, the probability of occurrence of an earthquake is weak.
机译:在上个世纪,印度发生了许多世界上最大的地震。实际上,该国超过50%的地区被认为容易发生破坏性地震。该国的东北地区以及整个喜马拉雅带都容易遭受8.0级以上的强烈地震。在这些地区发生地震的主要原因是印度板块每年向欧亚板块移动的速度约为50毫米。印度的地震分区图将印度划分为4个地震带(2区,3区,4区和5区)。根据当前的分区图,区域5的地震活动性最高,而区域2的地震活动性最低。在本文中,我们使用SAS(统计分析系统)和Weka(威卡托知识分析环境)这样的统计工具推导了地震震级频率数据集的回归关系。获得的回归关系是该区域的第一个关系。在地震灾害管理数据集中,幅度被视为因变量。它取决于LocationRank,StateRank,海拔,人口,年,月,日,小时,分钟,秒,纬度,经度和深度,它们被视为独立变量。基于因变量和自变量,可以在不同的地震位置分析新的“地震带”。如果大小等于或大于7,则大面积会根据其深度而损坏。如果震级等于或小于3,则地震发生的可能性很小。

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