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用F-K方法确定腾冲火山区震源机制*
引用本文:成瑾,陈培善,涂毅敏,刘瑞丰,白彤霞,中国北京. 用F-K方法确定腾冲火山区震源机制*[J]. 地震地磁观测与研究, 2000, 21(6): 1-10
作者姓名:成瑾  陈培善  涂毅敏  刘瑞丰  白彤霞  中国北京
作者单位:中国地震局地球物理研究所
基金项目:中国地震局“九五”火山项目!95-1 1 -0 2 -0 8,地震科学基金!1 991 1 6资助课题
摘    要:介绍了计算理论地震图的 F- K方法在不同深度 ,不同震中距 ,不同震源类型的情况 ,表明这种方法在高频区和多层水平层状模型计算效果较好 ,适用于研究中小地震的震源机制。采用 F- K方法得到了发生在腾冲火山区的 3个地震的震源机制 ,结果表明地震 1和地震 2是走滑断裂 ,地震 3是逆断层。 3个地震的主压应力轴基本呈北西向 ,与云南地区主压应力轴方向基本吻合 ,因此 ,推断这 3个地震是构造地震。

关 键 词:F-K方法  腾冲火山区  震源机制  构造地震

Source Estimation in tengchong volcano Area using F-K method
Cheng Jin,Chen Peishan,Tu Yimin,Liu Ruifeng and Bai Tongxia. Source Estimation in tengchong volcano Area using F-K method[J]. Seismological and Geomagnetic Observation and Research, 2000, 21(6): 1-10
Authors:Cheng Jin  Chen Peishan  Tu Yimin  Liu Ruifeng  Bai Tongxia
Abstract:The synthetic seismograms are computed by using F K method for a variety of conditions,such as various source types,relatively long range of epicentral distance and wide domain of frequency.The method can generally perform in a multi layered medium,and can be used for the purpose in the regional and local source mechanism.The source mechanism of the three earthquakes occurred in Tengchong volcano area is determined by this method.The result shows that the first event and the second event have strike slip faulting,and the third event has thrust faulting.The principal axis of compressive stress is oriented in NW direction,which tallies with the direction of tectonic field of Yunnan.It is inferred that they are tectonic earthquakes.
Keywords:F K method  Tengchong volcano area  source mechanism  tectonic earthquake
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