1.
Seismic Triggering and the Aftershock Distribution of the Wenchuan M8.0 Earthquake
汶川8.0级地震触发与余震活动空间分布研究
2.
A SIMPLE ANALYSIS OF WENCHUAN STRONG EARTHQUAKE SEQUENCE MOVING BASED ON ACTIVE TECTONIC BLOCK BOUNDARY ZONE
基于活动地块边界带的汶川强余震迁移分析
3.
The ratio of the precursory seismic quiescence area and the aftershock area of the great Tangshan mainshock is about0.7.
前兆地震活动平静区的面积与整个余震区面积之比值为0.7。
4.
The mobile strong-motion observation and preliminary analysis of typical records for Wenchuan aftershocks
汶川强余震流动观测与典型余震记录分析
5.
Strong ground motion observation for Wenchuan aftershocks
汶川M_S8.0地震的强余震流动观测
6.
Estimation on site effect from different techniques using aftershocks of Chi-Chi earthquake
利用集集地震余震记录分析场地地震动反应
7.
Relevant researches and developing tendency on the attenuation of frequency versus time of aftershocks, relation of magnitude-frequency and the development of stochastic simulation on seismic process have been mainly introduced and discussed.
重点介绍了余震衰减关系和震级、度关系的相关研究成果及地震活动过程随机模拟等的发展趋势。
8.
The Study on the Ground Motion Attenuation Law of Moderate Earthquake Area
中强地震活动区地震动衰减规律研究
9.
Using Active Source to Monitor Velocity Variation in Shallow Sediment Caused by the Wenchuan Earthquake
利用主动震源检测汶川地震余震引起的浅层波速变化
10.
Migration of the seismic activity is found before a big event.
发现了大震前地震活动性的迁移。
11.
Characteristics of seismic activity before 2008 Wenchuan M_S8.0 earthquake
2008年汶川M_S8.0地震前地震活动异常特征
12.
EFFECT OF WENCHUAN EARTHQUAKE ON SEISMIC ACTIVITY IN HUBEI
汶川地震对湖北地震活动趋势的影响
13.
Seismicity characteristics before the 2003 Chengkung,Taiwan,earthquake
2003年台湾成功地震前的地震活动特征
14.
Impact Analysis of the Seismic Activities of Circum-Pacific SEISMIC Belt
环太平洋地震带地震活动对中国大陆地震活动的影响分析
15.
making a hobby of domesticity.
做一种家庭生活的业余活动。
16.
Study on ground motion attenuation relationship of moderate earthquake risk areas
中强地震活动区地震动衰减关系的确定
17.
Study on Residual Shear Strength of Reinforced Concrete Bridge Columns under Strong Seismic Ground Movement;
强震动下钢筋混凝土桥墩的残余剪切强度研究
18.
Refraction First-Break Automatic Residual Static Corrections by Using Difference Method for the Seismic Wave Signals;
地震信号差分法初至折射波自动剩余静校正