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The Crustal Velocity Structure of Western Inner Mongolia
Zhao Yanhong,Jia Xiye
作者单位E-mail
Zhao Yanhong Earthquake Agency of Inner Mongolia Autonomous Region, Hohhot 010051, China  
Jia Xiye Baochang Seismic Station, Baochang 027099, Xilin Gol League, Inner Mongolia, China 728332829@qq.com 
摘要:
The terrain of Inner Mongolia is long and narrow, and the geological structure is complicated. The South China crustal velocity model and Inner Mongolia's optimal crustal velocity model 2015 cannot fully meet the earthquake location requirements of Inner Mongolia. Based on the seismological observations produced by Inner Mongolia Seismic Digital Network from 2009 to 2016, the initial model was obtained by using the linear fit of the seismic phases and the converted travel time curve. The Hyposat results of 225 earthquakes that occurred in western Inner Mongolia were scanned using this model, and the velocity model for western Inner Mongolia was determined as follows:V1=6.06km/s; VPb=6.61km/s; Vn=8.12km/s; H1=30m; and the Moho depth H=44km. Comparison of the test results of the new model and the reference model shows that the residual error of the new model and the mean deviation of the epicenter location have obviously decreased.
关键词:  Inner Mongolia Region  South China crustal velocity model  Optimal crustal velocity model of 2015  Western Inner Mongolia crustal velocity model
DOI:
分类号:
基金项目:This project was jointly funded by "Research, Development, Demonstration and Promotion Pilot Project of Earthquake Prediction and Early Warning Technology in Key Earthquake Areas" of the Science and Technology Major Projects of Inner Mongolia.
The Crustal Velocity Structure of Western Inner Mongolia
Zhao Yanhong,Jia Xiye
Abstract:
The terrain of Inner Mongolia is long and narrow, and the geological structure is complicated. The South China crustal velocity model and Inner Mongolia's optimal crustal velocity model 2015 cannot fully meet the earthquake location requirements of Inner Mongolia. Based on the seismological observations produced by Inner Mongolia Seismic Digital Network from 2009 to 2016, the initial model was obtained by using the linear fit of the seismic phases and the converted travel time curve. The Hyposat results of 225 earthquakes that occurred in western Inner Mongolia were scanned using this model, and the velocity model for western Inner Mongolia was determined as follows:V1=6.06km/s; VPb=6.61km/s; Vn=8.12km/s; H1=30m; and the Moho depth H=44km. Comparison of the test results of the new model and the reference model shows that the residual error of the new model and the mean deviation of the epicenter location have obviously decreased.
Key words:  Inner Mongolia Region  South China crustal velocity model  Optimal crustal velocity model of 2015  Western Inner Mongolia crustal velocity model