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The junction between the Dinarides and the Hellenides coincides with an orogenic bend characterized by a complex system of faults, domes and sedimentary basins. The major structure at this junction is the Shkoder-Peja Normal Fault (SPNF) system, whic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d6d34a139f01ae5824fd949cc7ffddde
https://doi.org/10.5194/egusphere-egu21-14816
https://doi.org/10.5194/egusphere-egu21-14816