Relationship between the earthquake sequences of Tangshan and Xingtai and the three dimensional velocity structure |
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Authors: | SHI-RONG MEI YAN XUE JING-YUAN YIN |
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Affiliation: | Center for Analysis and Prediction, China Seismological Bureau, Beijing 100036, China |
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Abstract: | In this paper, based on the results of tomographic image of Tangshan and Xingtai areas, the relations between the characteristics
of the two strong earthquake sequences and their three-dimensional velocity structures are studied. The research results indicate
that: (1) Mosaic distribution of low-velocity bodies and high-velocity bodies, especially the existence of high-velocity bodies
with large size in crust are the common basis of development of the two earthquake sequences. (2) Scale, depth, and heterogeneity
of high-velocity and low-velocity bodies are the important factors to effect the characteristic of earthquake sequences. (3)
The depth of the high-velocity body in Tangshan area is less than that in Xingtai area, which is the principal reason why
the dominant focal depth and the biggest focal depth of Tangshan earthquake sequence are less than Xingtai’s. (4) The depth
of the high-velocity bodies in Ninghe area is more than that in Tangshan-Luanxian area, which lead to the biggest magnitude
and epicentral intensity are lower. These results could be helpful for predicting the main shock of strong swarm-type earthquakes
and later strong aftershocks.
This project is supported by the Key Project from China Seismological Bureau under the Ninth Five-Year Plan (95-04-03-01-01). |
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Keywords: | strong earthquake sequence low-velocity anomalous body strong swarm-type earthquake dominant focal depth the biggest focal depth of aftershocks |
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