Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Marco Meda"'
Autor:
Daniel Barrera, Giovanni Toscani, Chiara Amadori, Marco Meda, Daniele Catellani, Maurizio Gorla, Andrea Di Giulio
Geothermal energy capacity in Europe has doubled in the last decade and will grow more over the next ten years, according to the 2020’s market report of the European Geothermal Energy Council. This brings great potential for development in Europe a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5108c915085a663eed2915fc744897d3
https://doi.org/10.5194/egusphere-egu23-13895
https://doi.org/10.5194/egusphere-egu23-13895
Autor:
Alessio Lucca, Silvia Mittempergher, Andrea Succo, Andrea Bistacchi, Marco Meda, Fabrizio Storti
The NW-SE striking Pag anticline, in the External Dinarides fold and thrust belt, provides an appropriate field site for studying fold- and fault-related deformation patterns at different scales in a transpressional setting due to outstanding exposur
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::76b4d1c43b8814602102a38608e8fb54
https://doi.org/10.5194/egusphere-egu23-5306
https://doi.org/10.5194/egusphere-egu23-5306
Autor:
Andreas Plesch, Alberto Cominelli, Lorenzo Osculati, Federica Caresani, Stefania Petroselli, Ruben Juanes, Marco Meda, David Castineira, Stefano Mantica, James H. Dieterich, F. Bottazzi, Bradford H. Hager, John H. Shaw, Cliff Frohlich
Publikováno v:
Nature. 595:684-689
There is growing concern about seismicity triggered by human activities, whereby small increases in stress bring tectonically loaded faults to failure. Examples of such activities include mining, impoundment of water, stimulation of geothermal fields
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5cc1dfdb8aefe505a6073198b4289fce
https://doi.org/10.1038/s41586-021-03668-z
https://doi.org/10.1038/s41586-021-03668-z
Autor:
Marco Meda, Silvia Mittempergher, Pierre Olivier Bruna, Andrea Bistacchi, Fabrizio Storti, Andrea Succo
Publikováno v:
Geological Field Trips. 11:1-19
The sedimentary succession exposed in the Northern Dalmatia Islands mainly consists of Cretaceous to Neogene shallow water carbonates, folded and imbricated within the External Dinarides thrust belt. During Cretaceous times, carbonate sediments were
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6475727f527331f9c280c3772835273a
https://doi.org/10.3301/gft.2019.06
https://doi.org/10.3301/gft.2019.06
Publikováno v:
Tectonics. 38:3394-3415
The tectonic and geodynamic evolution of the Pelagian platform and of the Pantelleria Rift System, located in the foreland of the Apennine-Sicilian-Maghrebian Belt, from the Late Oligocene onward, is still debated. Here we present a new interpretatio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0e725d7c179b911f4274b41d5550e394
https://doi.org/10.1029/2019tc005627
https://doi.org/10.1029/2019tc005627
Autor:
Gregoire Mariethoz, Marco Meda, Pierre-Olivier Bruna, Julien Straubhaar, Kevin Bisdom, Rahul Prabhakaran, Giovanni Bertotti
Publikováno v:
Solid Earth, 10(2)
Solid Earth, Vol 10, Pp 537-559 (2019)
Solid Earth, Vol 10, Pp 537-559 (2019)
Natural fracture network characteristics can be establishes from high-resolution outcrop images acquired from drone and photogrammetry. Such images might also be good analogues of subsurface naturally fractured reservoirs and can be used to make pred
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9875c090f2e4c6af5094772221b95b53
https://doi.org/10.5194/se-10-537-2019
https://doi.org/10.5194/se-10-537-2019
Autor:
Fabrizio Balsamo, Fabrizio Storti, Silvia Mittempergher, Andrea Bistacchi, Marco Meda, Luigi Berio
In many orogenic wedges, foreland basin systems are preferential sites for economical resource accumulation, typically hydrocarbons. Understanding how structural inheritance perturbs the evolution of folding-related deformation and impacts on subsurf
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5f8cfc0b57372784bf0771b10ee67d63
http://hdl.handle.net/10281/335192
http://hdl.handle.net/10281/335192
Autor:
Andrea Bistacchi, François Bonneau, Marco Meda, Mattia Martinelli, Fabrizio Balsamo, Silvia Mittempergher, Guillaume Caumon
Publikováno v:
Journal of Structural Geology
Journal of Structural Geology, Elsevier, 2020, 140, pp.104144. ⟨10.1016/j.jsg.2020.104144⟩
Journal of Structural Geology, Elsevier, 2020, 140, pp.104144. ⟨10.1016/j.jsg.2020.104144⟩
International audience; Fault damage zones can act as a preferential corridor for fluid flow in the subsurface, and for this reason the characterization of their structure, including the attributes of the associated fracture network, is fundamental.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::873c61ab1279f91b65be7e5ba194eaae
http://hdl.handle.net/10281/281244
http://hdl.handle.net/10281/281244
Autor:
Cristian Cavozzi, Roberto Longoni, Marco Meda, Corrado Magistroni, Fabrizio Righetti, Yago Nestola, Paolo D’Adda, Fabrizio Storti
Publikováno v:
Interpretation. 5:SD55-SD66
The structural framework of the Val d’Agri region results from the superposition of different deformation events over time. In this area, the largest European onshore oil field was discovered in the 1980s, and since then, much geologic and geophysi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::155451340dca070a75f1f425a21cac4a
https://doi.org/10.1190/int-2016-0078.1
https://doi.org/10.1190/int-2016-0078.1
Autor:
Pierre-Olivier Bruna, Julien Straubhaar, Rahul Pranhakaran, Giovanni Bertotti, Kevin Bisdom, Grégoire Mariethoz, Marco Meda
Natural fractures have a strong impact on flow and storage properties of reservoirs. Their distribution in the subsurface is largely unknown mainly due to their sub-seismic scale and to the scarcity of available data sampling them (borehole). Outcrop
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::33f0a8ddaae132c18d039106fc6e442c
https://doi.org/10.5194/se-2018-106
https://doi.org/10.5194/se-2018-106