Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Manuel Diercks"'
Publikováno v:
Geologija, Vol 65, Iss 1, Pp 93-99 (2022)
In our paper Diercks et al. (2021) we presented geomorphological data and field observations from W Slovenia and NE Italy to develop a model for the formation of the Pradolino (slov. Pradol) dry valley. After publication we were kindly pointed to exi
Externí odkaz:
https://doaj.org/article/996f7697fb2647ddb4dbbe87f73b3a2c
Publikováno v:
Geologija, Vol 64, Iss 1, Pp 21-33 (2021)
In tectonically active mountain ranges, the landscape is shaped by the interplay of erosion/sedimentation and tectonically driven crustal deformation. Characteristic landforms such as moraines, wind gaps, fault scarps, and river terraces can be use
Externí odkaz:
https://doaj.org/article/96dd925abba74958b8b6e2a1991c4327
Publikováno v:
Geosciences, Vol 10, Iss 2, p 84 (2020)
The NW-SE trending Udine-Buttrio Thrust is a partly blind fault that affects the Friulian plain southeast of Udine in NE Italy. It is part of a wider fault system that accommodates the northward motion of the Adriatic plate. Although seismic reflecti
Externí odkaz:
https://doaj.org/article/6f3dd377085445ccb67cfcae2cebd0dd
Knowledge of earthquake source faults is crucial to calculate robust Coulomb stress models. However, source faults are often poorly constrained, especially for pre-instrumental events, and these historic earthquakes are commonly studied with little o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5deb4c2d931ef486a2aceb15286156da
https://doi.org/10.22541/essoar.168057577.71492202/v1
https://doi.org/10.22541/essoar.168057577.71492202/v1
Publikováno v:
Geologija, Vol 64, Iss 1, Pp 21-33 (2021)
In tectonically active mountain ranges, the landscape is shaped by the interplay of erosion/sedimentation and tectonically driven crustal deformation. Characteristic landforms such as moraines, wind gaps, fault scarps, and river terraces can be used
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f17d23c03fbeb7b99e7d880491faa325
https://doi.org/10.5474/geologija.2021.002
https://doi.org/10.5474/geologija.2021.002
Publikováno v:
Geosciences
Volume 10
Issue 2
Geosciences, Vol 10, Iss 2, p 84 (2020)
Geosciences 10(2), 84 (2020). doi:10.3390/geosciences10020084 special issue: "Special Issue "Seismic Sequence in Mediterranean Region" / Special Issue Editors: Dr. Giovanni Lanzano, Guest Editor; Dr. Stefano Pucci, Guest Editor; Dr. Sara Sgobba, Guest Editor; Dr. Salvatore Grasso, Co-Guest Editor"
Volume 10
Issue 2
Geosciences, Vol 10, Iss 2, p 84 (2020)
Geosciences 10(2), 84 (2020). doi:10.3390/geosciences10020084 special issue: "Special Issue "Seismic Sequence in Mediterranean Region" / Special Issue Editors: Dr. Giovanni Lanzano, Guest Editor; Dr. Stefano Pucci, Guest Editor; Dr. Sara Sgobba, Guest Editor; Dr. Salvatore Grasso, Co-Guest Editor"
The NW-SE trending Udine-Buttrio Thrust is a partly blind fault that affects the Friulian plain southeast of Udine in NE Italy. It is part of a wider fault system that accommodates the northward motion of the Adriatic plate. Although seismic reflecti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e6688f1adc408e100ce5060419278819
https://doi.org/10.3390/geosciences10020084
https://doi.org/10.3390/geosciences10020084