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Publikováno v:
European Journal of Environment and Earth Sciences. 4:1-5
During the last five decades since 1968, the Elbasani zone in Albania is dominated by low seismicity. This fault zone has evidenced some seismological phenomena. It is a transversal active fault zone with normal and strike-slip faults characterized b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1c614b69326557ed8ccb302555f245a2
https://doi.org/10.24018/ejgeo.2023.4.2.380
https://doi.org/10.24018/ejgeo.2023.4.2.380
