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内蒙古东部地区一维地壳速度结构分析

赵艳红 张帆 娜热

地震地磁观测与研究2018,Vol.39Issue(1):41-48,8.
地震地磁观测与研究2018,Vol.39Issue(1):41-48,8.DOI:10.3969/j.issn.1003-3246.2018.01.007

内蒙古东部地区一维地壳速度结构分析

Study on 1D crustal velocity structure in the eastern of Inner Mongolia

赵艳红 1张帆 1娜热1

作者信息

  • 1. 中国呼和浩特 010051 内蒙古自治区地震局
  • 折叠

摘要

Abstract

Based on the data of 131 seismic data recorded in the eastern part of Inner Mongolia from 2009 to 2016, the velocity model of the eastern part of Inner Mongolia was obtained by using the method of "velocity fitting, zoning and folding". v1 = 6.10 km/s, vPb = 6.72 km/s, vn = 8.05 km/s, H1 = 23 m and H2 = 16 km. The results of the eastern model show that the mean of the residuals in the eastern model is significantly lower than that of the South China model and the 2015 Inner Mongolia optimal model, and the residuals are more uniform and stable. The epicenter difference of "East model - catalog" is less 1 km than those of "South China - catalog", "2015 Inner Mongolia optimal model - catalog" and "South China - catalog" . It can be seen that the eastern model more suitable for eastern region of Inner Mongolia.

关键词

内蒙古东部地区/华南模型/2015内蒙最优模型/东部模型

Key words

eastern of Inner Mongolia region/South China model/the optimal model 2015 in Inner Mongolia/the model in the east

引用本文复制引用

赵艳红,张帆,娜热..内蒙古东部地区一维地壳速度结构分析[J].地震地磁观测与研究,2018,39(1):41-48,8.

基金项目

内蒙古自治区地震局局长基金课题(项目编号:2016JC05) (项目编号:2016JC05)

内蒙古自治区科技重大专项"重点地区地震预测预警技术研究开发与推广示范" ()

地震地磁观测与研究

1003-3246

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