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强震临震微波动:来自于震源的信息?

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简要回顾了强震临震微波动研究的科学问题、分析思路、主要特征和多年实时震情跟踪实践结果,总结了临震微波动主要特征,表现为:①优势频率为11~16 Hz,频谱形态较为整齐;②可能出现在震前2~24d,可以被震中距70 km半径范围内的台站记录到;③具有重现性,在多次强震前出现;④可能与震级有关,震级越大,震前出现临震微波动的可能性越大.介绍了 2021年云南漾濞6.4级地震和2021年青海玛多7.4级地震余震活动阶段观测到临震微波动的新结果,做出了强震临震微波动可能来自于震源区或地震破裂带的推测.
Microfluctuations in Impending Strong Earthquakes:Information from the Hypocentral Area?
This paper briefly reviews the scientific issues,analytical methods,main fea-tures,and results of years of real-time earthquake tracking practice on impending strong earthquake microfluctuations.The main characteristics of impending earthquake mi-crofluctuations are summarized as follows:① The dominant frequency is 11~16 Hz,and the spectrum shape is relatively neat;② It may appear 2~24 days before the earthquake,and can be recorded by stations within a radius of 70 km of the epicenter;③ It is repro-ducible and appears before multiple strong earthquakes;④ It may be related to the magni-tude of the earthquake.The greater the magnitude,the greater the possibility of impend-ing earthquake microfluctuations before the earthquake.This paper introduces the new re-sults of microfluctuations observed during the aftershock activity of the 2021 Yangbi M6.4 earthquake and the 2021 Maduo M7.4 earthquakes.It is inferred that the microfluctua-tions of imminent strong earthquakes may originate from the hypocentral area or the earth-quake rupture zones.

Strong earthquakesMicrofluctuations of imminentDominant frequency 11~16 HzReproducibilityOriginating from earthquake source hypocentral areaEarthquake rupture zone

杨立明、王建军、郝臻

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中国地震局第二监测中心,陕西西安 710054

甘肃省地震局,甘肃兰州 730000

强震 临震微波动 优势频率11~16 Hz 重现性 来源于震源区 地震破裂带

2024

地震
中国地震局地震预测研究所 中国地震学会地震预报专业委员会 中国地震学会地震流体专业委员会 中国地震学会地震电磁学专业委员会

地震

CSTPCD北大核心
影响因子:0.733
ISSN:1000-3274
年,卷(期):2024.44(4)