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| 引用本文： | 刘冬英. ����̨ˮ�¡�ˮ��쳣���봨8.0�������ϵ̽��[J]. 大地测量与地球动力学, 2008, 28(6): 53-55 |
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| 作者姓名： | 刘冬英 |
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| 作者单位： | 中国地震局地壳应力研究所,北京,100085 |
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| 基金项目： | 中国地震局地壳应力研究所基本科研业务专项基金 ， 国家科技支撑计划 |
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| 摘 要： | ???????8.0???????????????????????????????н?1 800???????????????????o??????????????????????????????????????????????8.0???????й??
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| 关 键 词： | ????????? ??? ?? ?? ??8.0?????? |
DISCUSSION ON RELATION BETWEEN ANOMALIES OF WATER TEMPERATURE AND RADON IN NINGBO STATION AND WENCHUAN Ms8.0 EARTHQUAKE |
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| Liu Dongying. DISCUSSION ON RELATION BETWEEN ANOMALIES OF WATER TEMPERATURE AND RADON IN NINGBO STATION AND WENCHUAN Ms8.0 EARTHQUAKE[J]. Journal of Geodesy and Geodynamics, 2008, 28(6): 53-55 |
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| Authors: | Liu Dongying |
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| Affiliation: | Institute of Crustal Dynamics, CEA, Beijing 100085 |
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| Abstract: | Anomaly data of underground water were and analyzed after Wenchuan Ms8.0 earthquake in 12th May, 2008. Before earthquake accured, there were some anomalies of water temperature and radon in Ningbo station of Zhejiang province, which is 1 800 km away from epicenter. By carrying out the well condition, through contrasting this data with previous ones and analyzing them,it is thought that these anomalies were related to Wenchuan Ms8.0 earthquake. |
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| Keywords: | Ningbo station water temperature water radon anomaly Wenchuan Ms8.0 earthquake |
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