Pathways of volatile migration in the crust beneath Harrat Lunayyir (Saudi Arabia) during the unrest in 2009 revealed by attenuation tomography
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文摘
We present P and S wave attenuation models beneath Harrat Lunayyir (Saudi Arabia). We use the t* measurements for events recorded during an unrest in April–June 2009. P and S models reveal the same high-attenuation zone in the upper crust. This zone marked by seismicity possibly indicates the pathway of gas output. The cause of the Lunayyir unrest is a volatile injection from a deep magma source.

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