Zobrazeno 1 - 10
of 31
pro vyhledávání: '"Antonio Luca Funedda"'
Autor:
Antonio Luca Funedda, Fabrizio Cocco
Publikováno v:
Geosciences, Vol 11, Iss 276, p 276 (2021)
Geosciences
Volume 11
Issue 7
Geosciences
Volume 11
Issue 7
Fold-and-thrust belts have a high variability of structural styles, whose investigation provides continuous updates of the predictive models that try to better approximate the geometries recognized in the field. The majority of studies are focused on
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::32e3c384384aae0ed3419ef6c3c2f638
https://www.mdpi.com/2076-3263/11/7/276
https://www.mdpi.com/2076-3263/11/7/276
Autor:
Filippo Mundula, Anna Gioncada, Raffaello Cioni, Antonio Luca Funedda, Marco Lezzerini, Paolo Fulignati, E. Pitzalis
Publikováno v:
Geoheritage. 11:1567-1581
Spectacular volcanic landforms characterize the Miocene lava flows and ignimbrites forming San Pietro Island (Sardinia, Italy). The island, furthermore, is a site of volcanic-hosted manganese mineralizations, which have been exploited until the past
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ab35b3fd77c28758445c789d2ed7c14a
https://doi.org/10.1007/s12371-019-00418-6
https://doi.org/10.1007/s12371-019-00418-6
Publikováno v:
Terra Nova. 31:485-493
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::afca17b51628e314fdb536ca34cd63e1
https://doi.org/10.1111/ter.12418
https://doi.org/10.1111/ter.12418
Autor:
Antonio Luca Funedda, Fabrizio Cocco
The Variscan foreland of SW-Sardinia consists of a Cambrian to lower Carboniferous succession polydeformed under very low-grade metamorphism. It is characterized by the following superposed structures: 1) E-W-trending upright folds; 2) N-S-trending i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0fb4b91bb56874bd3eeef69db4ba27d0
https://doi.org/10.5194/egusphere-egu21-9034
https://doi.org/10.5194/egusphere-egu21-9034
Autor:
Fabrizio Cocco, Dario Fancello, Matteo Deidda, Antonio Attardi, Antonio Luca Funedda, Stefano Naitza
The Rosas Shear Zone (RSZ) is a 1 km thick brittle-ductile shear zone that outcrops in the Variscan fold and thrust belt foreland of SW Sardinia, where several important ore deposits were mined in the last century. The RSZ lies in the footwall and st
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::26aef5f30c980ee195014acc70bd9401
https://doi.org/10.5194/egusphere-egu21-2806
https://doi.org/10.5194/egusphere-egu21-2806
Autor:
Raúl Carrey, Neus Otero, Giorgio Ghiglieri, Claudio Arras, Cristina Buttau, Cristina Domènech, Albert Soler, Clara Torrentó, Alberto Carletti, Manuela Barbieri, Antonio Luca Funedda
Publikováno v:
Dipòsit Digital de la UB
Universidad de Barcelona
Universidad de Barcelona
This study presents a multi-disciplinary approach for the hydrogeological assessment and characterization of water resources in typical arid and semi-arid areas with high anthropogenic pressure, and where environmental conditions and political contex
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::47889fd6b383aa2cc556d62bcda0a77b
https://pubmed.ncbi.nlm.nih.gov/33288271
https://pubmed.ncbi.nlm.nih.gov/33288271
Autor:
Ivan Erbì, Giacomo Deiana, Stefania Da Pelo, Marco Loche, Valentino Demurtas, Maria Teresa Melis, Gianvito Scaringi, F. Dessì, Marco Scaioni, Mattia Alessio Meloni, Antonio Luca Funedda
Publikováno v:
Remote Sensing, Vol 12, Iss 1971, p 1971 (2020)
Coastal retreat is a non-recoverable phenomenon that—together with a relevant proneness to landslides—has economic, social and environmental impacts. Quantitative data on geological and geomorphologic features of such areas can help to predict an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f2f6101f8f1224f8017b2eb805c0c157
https://www.mdpi.com/2072-4292/12/12/1971
https://www.mdpi.com/2072-4292/12/12/1971
Publikováno v:
Journal of Iberian Geology. 44:619-639
The Variscan Palaeozoic successions exposed in Sardinia show clear evidences of tectonic instability during Ordovician times. In the Foreland zone (SW Sardinia), the Cambrian to lower Ordovician strata are folded giving way to an angular unconformity
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::19a808f6571eea637c904bc39ff7f480
https://doi.org/10.1007/s41513-018-0075-1
https://doi.org/10.1007/s41513-018-0075-1
Publikováno v:
Sedimentary Geology. 361:64-81
The Chattian-Aquitanian carbonate system of Isili sub-basin (SE Sardinia, Italy) were studied to better understand the hydrodynamic processes controlling the formation of landward-downlapping, rhodolith-rich, giant clinoforms. The studied flat-topped
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f351d17c2bb4840d0450c251a54d846d
https://doi.org/10.1016/j.sedgeo.2017.09.012
https://doi.org/10.1016/j.sedgeo.2017.09.012
Autor:
Antonio Luca Funedda, Fabrizio Cocco
Publikováno v:
Geological Magazine. 156:25-38
Detailed geological mapping, field observations and structural analyses demonstrate that Early Ordovician (‘Sardic’) deformation occurred in the early Palaeozoic successions that are now incorporated in the Variscan Nappe zone of SE Sardinia. Thi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0591a47de88ffba8c0f5a7786df5f360
https://doi.org/10.1017/s0016756817000723
https://doi.org/10.1017/s0016756817000723