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利用合成地震图研究东北地区壳幔介质结构
引用本文:林美,龚绍京.利用合成地震图研究东北地区壳幔介质结构[J].地震学报,1991,13(4):480-488.
作者姓名:林美  龚绍京
作者单位:1. 中国石家庄 050021 河北省地震局 2. 中国北京 100101 中国科学院地球物理研究所
摘    要:本文采用计算合成地震图与分布在东北地区的11个地震台记录的深源远震波形对比分析的方法,研究该区壳幔结构.结果表明,东北地区地下100km 以上壳幔介质为分层结构,并存在有低速层.莫霍界面较清晰.地壳厚度在31.8——35.8km 之间. 

关 键 词:合成地震图    深源远震波形    东北介质结构

A STUDY OF CRUST AND UPPER MANTLE STRUCTURE IN THE NORTHEASTERN REGION OF CHINA BY MEANS OF SYNTHETIC SEISMOGRAMS
Affiliation:1. Seismological Bureau of Hebei Province, Shijiazhuang 050021, China; 2. Institute of Geophysics, Academia Sinica, Beijing 100101, China
Abstract:In this paper, structure models of the crust and upper mantle beneath each station have been obtained by way of fitting synthetic seismograms with P waveforms of deep focus teleseismic records from the 11 stations in the Northeastern Region of China. We have studied the structure in the region based on those models. Our results show that the medium of the crust and upper mantle is a layered structure with alternate high and low velocity layers within about 100 km under the region. The crustal thickness is about 31.8-35.8km. 
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