1.
Study on the IASPEI New Body Wave Magnitude Standards
IASPEI新标准体波震级分析研究
2.
There are two chief kinds of seismic waves: body waves and surface waves.
有两种主要的地震波：体波和面波。
3.
The relation between soures S wave acceleration and magnitude is discussed.
并探讨了震源S波加速度与震级的关系.
4.
ANOMALOUS VARIATIONS OF THE CHARACTERITICS OF SEISMIC WAVES BEFORE THE TANGSHAN(唐山) STRONG EARTHQUAKE(M=7.8)
唐山7.8级强震前地震波特性的异常变化
5.
CERTAIN SHORT TERM ANOMALOUS VARIATIONS OF THE CHARACTERISTICS OF SEISMIC WAVES BEFORE THE KUERLE EARTHQUAKE ( M=5.8)
库尔勒5.8级地震前地震波特性的某些短期变化
6.
The Coda Wave Attenuation Characteristics in 1830 Cixian,M7.5 Earthquake Area
1830年磁县7.5级地震震源区尾波衰减特征
7.
STATISTICAL TEST OF PRECURSORY WAVES BEFORE WENCHUAN Ms8.0 EARTHQUAKE
汶川8.0级地震前驱波的统计检验
8.
Long-Wave-Radiation Patterns prior to the Wenchuan M8.0 Earthquake
汶川8.0级大地震的长波辐射征象
9.
An earthquake with a magnitude of less than 2.0 is so slight that usually only a seismometer can detect it.
小于2.0震级的地震非常轻微，通常只有地震检波器才能探测到。
10.
THE PHENOMENON OF CO-SEISM CHANGE ABOUT WATER LEVEL AND THE TILE OF NINGBO SEISMIC STATION IN INDONESIA EARTHQUAKES WITH M_S8.7 AND M_S8.5
宁波地震台水位、地倾斜在印尼8.7、8.5级地震中的同震变化现象
11.
Study on Automatic Recognition of Seismic Arriving Time and Rapid Estimation of Magnitude in Earthquake Early Warning;
地震预警中地震波到时自动识别和震级快速估算研究
12.
Wenchan Ms8.0 Earthquake Coseismic Effects in ZK03 Well and VS Vertical Pendulum Tiltmeter of Ningbo Seismic Station
宁波地震台动水位与垂直摆对汶川8.0级地震的同震变化
13.
Body waves, the fastest seismic waves, move through the earth.
体波是最快的地震波，可贯穿地球。
14.
Discussion on Relationship between Fluid Anomalies at Tianshui Station and Wenchuan 8.0 Earthquake
天水地震台流体异常与汶川8.0级地震关系探讨
15.
Variation characteristic of some seismic wave parameters before the Yangjiang earthquake with M4.2 on April 22,2001
2001年4月22日阳江4.2级地震前部分地震波参数变化特征
16.
A STUDY OF THE MEDIUM FEATUR E AND SOURCE SUB WAVE OF THE WUQIA EARTHQUAKE OF M=7.4 ON AUGUST 23, 1985 USING HOMOMORPHIC DECONVOLUTION
用同态反褶积研究1985年乌恰7.4级地震的震源子波以及介质特性
17.
A STUDY ON SOURCE PROCESS OF M S 6.8 EARTHQUAKE IN XIJIE, QINGHAI PROVINCE OF NOVEMBER 5,1988 BY USING BROADBAND DIGITAL SEISMIC WAVE DATA
用宽频带波形资料研究青海西捷6.8级地震的震源过程
18.
DISCUSSION ON SEISMIC VELOCITY ANOMALIES OF LONGMENSHAN FAULT ZONE AFTER WENCHUAN 8.0 EARTHQUAKE
汶川8.0级地震后龙门山断裂地震波速异常的讨论