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Autor:
Haridhi Haekal A., Huang Bor Shouh, Faizi Muhammad, Ramadhan Putri, Harahap Ridrya A.A., Ismanto Nurhadi, Sianipar Dimas
Publikováno v:
E3S Web of Conferences, Vol 447, p 01013 (2023)
The high-frequency seismic waves are usually generated by shallow earthquakes and is observed at a location near the earthquake source. Seismic energy tends to attenuate as it propagates through the Earth’s surface and interior; however, this is no
Externí odkaz:
https://doaj.org/article/947b6d594aaf42d288f77d056ab29714
