浅析太原台记录太原盆地地震波形的特征
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
选用太原台DD-1仪记录到的太原盆地多种波形并将其整理归纳,总结出了横穿和纵穿盆地到达记录台站的两种波形特点,并分析了它们呈现该特征主要是源于波在传播过程中地壳厚度分布不均、震源机制以及各种波本身的物理性质不同而造成的。
We processed various waveform data that recorded by the DD - 1 seismograph installed in Taiyuan Seismic Station, and found the waveform characteristics of two kinds of waves that propagate through Taiyuan basin transversely and longitudinally, respectively. We conluded that the waveform characteristics can be owing to the thickness variation of the crust where the waves propagate through and the difference in the focus mechanism and physical properts of various waves.
引文
国家地震局地球物理研究所.1997.近震分析[M].北京:地震出版社
    徐国明,周慧兰.1982.地震学原理[M].北京:科学出版社
    赵荣国.1980.中国地震台站地震记录图集[M].北京:地震出版社

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心