Source time-function as discriminant using empirical Green's function  

Source time-function as discriminant using empirical Green’s function

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作  者:HE Yongfeng1,2 & CHEN Xiaofei1 1. Department of Geophysics, School of Earth & Space Sciences, Peking University, Beijing 100871, China 2. North-West Institute of Nuclear Technology, Xi’an 710024, China 

出  处:《Science China Earth Sciences》2005年第12期2118-2122,共5页中国科学(地球科学英文版)

基  金:This work was partially supported by the National Nature Science Foundation of China(Grant No.40134010).

摘  要:The source mechanism of underground nuclear explosions is remarkably different from that of earthquakes in both spatial radiation pattern and source time-function (STF). Small underground nuclear explosions can be used as empirical Green’s functions (EGF) to isolate the source-time spectrum of a large suspected earthquake occurred in a Nuclear Test Site (target area) by the spectral division method. As this study shows, with high-quality data, the quotient spectrum can be transformed to the time domain, yielding the apparent far-field source-time function of the large suspected event. The relative source time-function (RSTF) of a nuclear ex-plosion is usually a simple pulse with a duration of about 1 s., while an earthquake’s is more complicated with a series of pulses and a longer duration. The RSTF can be used as a nice dis-criminant to distinguish the nature earthquakes from underground nuclear explosions in target areas.The source mechanism of underground nuclear explosions is remarkably different from that of earthquakes in both spatial radiation pattern and source time-function (STF). Small underground nuclear explosions can be used as empirical Green’s functions (EGF) to isolate the source-time spectrum of a large suspected earthquake occurred in a Nuclear Test Site (target area) by the spectral division method. As this study shows, with high-quality data, the quotient spectrum can be transformed to the time domain, yielding the apparent far-field source-time function of the large suspected event. The relative source time-function (RSTF) of a nuclear ex-plosion is usually a simple pulse with a duration of about 1 s., while an earthquake’s is more complicated with a series of pulses and a longer duration. The RSTF can be used as a nice dis-criminant to distinguish the nature earthquakes from underground nuclear explosions in target areas.

关 键 词:target-area  empirical Green's function  RSTF. 

分 类 号:O174[理学—数学]

 

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