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Electrical resistivity tomography (ERT) and ground-penetrating radar (GPR) are frequently used geophysical methods in the exploration of near-surface targets such as archaeological features. These methods were therefore appl
Electrical resistivity tomography (ERT) and ground-penetrating radar (GPR) are frequently used geophysical methods in the exploration of near-surface targets such as archaeological features. These methods were therefore appl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::de66659b0fb85fe3d7e79e57281bc55d
https://hdl.handle.net/11421/14030
https://hdl.handle.net/11421/14030