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Abstract Strong mining-induced earthquakes in deep mines threaten surface infrastructure, yet their surface vibration fields are difficult to predict because propagation paths cross goafs, fractured overburden, and variable Quaternary cover. This study used a dense surface monitoring array at the Dongtan Coal Mine to characterize the time–frequency evolution and spatial attenuation of typical mining-induced seismic events.
As a journalist, you can create a free Muck Rack account to customize your profile, list your contact preferences, and upload a portfolio of your best work.
