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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
Autor:
Grund, Marc U.1 (AUTHOR) m.grund@fu-berlin.de, Handy, Mark R.1 (AUTHOR), Giese, Jörg2,3 (AUTHOR), Gemignani, Lorenzo1 (AUTHOR), Pleuger, Jan1 (AUTHOR), Onuzi, Kujtim4 (AUTHOR)
Publikováno v:
International Journal of Earth Sciences. Sep2023, Vol. 112 Issue 6, p1613-1634. 22p.
Autor:
Grund, Marc U.1 (AUTHOR), Giese, Joerg1,2 (AUTHOR), Zertani, Sascha1 (AUTHOR), Handy, Mark R.1 (AUTHOR), Pleuger, Jan1 (AUTHOR), LeBreton, Eline1 (AUTHOR), Onuzi, Kujtim3 (AUTHOR)
Publikováno v:
Geophysical Research Abstracts. 2019, Vol. 21, p1-1. 1p.