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| 1 | Advances in research on earthquake fluids hydrogeology in China:a review显示文摘Monitoring of subsurface fluid(underground fluid)is an important part of efforts for earthquake prediction in China.The nationwide network,which monitors groundwater level,water temperature,and radon and mercury in groundwater,has been constructed in the last decades.Large amounts of abnormal fluid changes before and after major earthquakes have been recorded,providing precious data for research in earthquake sciences.Many studies have been done in earthquake fluid hydrogeology in order to probe the nature of the earthquake.Much progress in earthquake fluid hydrogeology has been made in the last decades.The paper provides a review of the advances in research on earthquake fluid hydrogeology over the last40 years in China.It deals with the following five aspects:(1)an introduction to the development history of monitoring networks construction;(2)cases of different subsurface fluid changes recorded before some majorearthquakes which occurred in the last decades;(3)characteristics of subsurface fluid changes following major earthquakes;(4)mechanism of subsurface fluid changes before and following earthquakes;(5)application of earthquake fluids in the hydrogeology field. | Zheming Shi Guangcai Wang Chenglong Liu | 2013 | Earthquake Science2013，26，6： | 3 |
| 2 | 新闻报道中的部分禁用词显示文摘1.对有身体残疾的人士不使用“残废人”、“瞎子”、“聋子”、“弱智”等蔑称,而应使用“残疾人”、“盲人”、“聋人”、“智力障碍者”等词语。 | | 2014 | 国际免疫学杂志2014，37，2： | 0 |
| 3 | A theoretical study of correlation between scaled energy and earthquake magnitude based on two source displacement models显示文摘The correlation of the scaled energy,e?=Es/M0,versus earthquake magnitude,Ms,is studied based on two models:(1)Model 1 based on the use of the time function of the average displacements,with a x-2source spectrum,across a fault plane;and(2)Model 2 based on the use of the time function of the average displacements,with a x-3source spectrum,across a fault plane.For the second model,there are two cases:(a)As s*T,where s is the rise time and T the rupture time,lg(e?)*-Ms;and(b)As s T,lg(e?)*-(1/2)Ms.The second model leads to a negative value of e?.This means that Model 2 cannot work for studying the present problem.The results obtained from Model 1 suggest that the source model is a factor,yet not a unique one,in controlling the correlation of e?versus Ms. | Jeen-Hwa Wang | 2013 | Earthquake Science2013，26，6： | 0 |
| 4 | 学术交流活动显示文摘 | 孙玥 | 2013 | 天津音乐学院学报2013，，4： | 0 |
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