爆炸、核试验与天然地震的区别（英文）

本文通过地震正演模型和面波振幅数据对比分析了天然地震、爆炸,与核试验数据,以探索改进辨别天然地震与爆炸的方法。所提方法是基于波数域和频率域的双积分变换解。用于研究的地震事件都发生在北朝鲜,其中包括2001年6月26日（39.212°N,125.383°E）和2001年10月30日（38.748°N,125.267°E）所记录的爆炸数据,2006年10月9日（41.275°N,129.095°E）所记录的一次核试验数据、以及2002年4月14日（39.207°N,125.686°E）和2002年6月7日（38.703°N,125.638°E）所记录的两次天然地震。基于这些数据通过地震波分析与理论模拟表明爆炸引起的地震与天然地震有着不同的波型特征。爆炸引起的信号特征是P波的能量较S波强,在爆炸记录上0.05-0.5Hz频率之间Rg波清晰呈现,而在然地震记录上没有。这是由于爆炸地震记录上P波是优势波,与SH成分发生了耦合。

Discriminating between explosions and earthquakes

Earthquake, explosion, and a nuclear test data are compared with forward modeling and band-pass filtered surface wave amplitude data for exploring methodologies to improve earthquake–explosion discrimination. The proposed discrimination method is based on the solutions of a double integral transformation in the wavenumber and frequency domains. Recorded explosion data on June 26, 2001（39.212°N, 125.383°E） and October 30, 2001（38.748°N, 125.267°E）, a nuclear test on October 9, 2006（41.275°N, 129.095°E）, and two earthquakes on April 14, 2002（39.207°N, 125.686°E） and June 7, 2002（38.703°N, 125.638°E）, all in North Korea, are used to discriminate between explosions and earthquakes by seismic wave analysis and numerical modeling. The explosion signal is characterized by first P waves with higher energy than that of S waves. Rg waves are clearly dominant at 0.05–0.5 Hz in the explosion data but not in the earthquake data. This feature is attributed to the dominant P waves in the explosion and their coupling with the SH components.