Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Ivano Dini"'
Autor:
Cora Dutsch, Ivano Dini, Stefan Buske, Simonetta Ciuffi, Catherine Alexandrakis, Marko Riedel
Publikováno v:
Geophysical Prospecting. 63:957-974
This work represents a case study concerning the application of reflection seismic imaging methods in the context of geothermal exploration. Our goal is to obtain accurate structural images of a geothermal active area in southern Tuscany. These image
Autor:
Martin Thorwart, Gabriele Marquart, Jan Niederau, Anozie Ebigbo, Ruggero Bertani, Ivano Dini, Renate Pechnig, Wolfgang Rabbel, Christoph Clauser
Publikováno v:
Geothermal Energy, 4
Geothermal Energy 4(1), 5 (2016). doi:10.1186/s40517-016-0047-7
Geothermal Energy 4(1), 5 (2016). doi:10.1186/s40517-016-0047-7
Granitoid intrusions are the primary heat source of many deep geothermal reservoirs in Tuscany. The depth and shape of these plutons, characterised in this study by a prominent seismic reflector (the K horizon), may vary significantly within the spat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1725719eb7405123fee5f827286257b8
https://hdl.handle.net/20.500.11850/125877
https://hdl.handle.net/20.500.11850/125877
Autor:
Fausto Batini, Alexandre Throo, Charles Naville, Fabio Cecconi, Ivano Dini, Sylvain Serbutoviez
Publikováno v:
All Days.
Development drilling occurs sometimes in areas where the surface seismic quality is poor. Drilling in such areas is risky enough to justify the application of drillbit SWD for seismic illumination ahead of the bit. A multidisciplinary project partial
Publikováno v:
SEG Technical Program Expanded Abstracts 1994.
VSP data were collected in the Larderello geothermal field in Italy in order to attempt to image reflective features below the depth of current geothermal production with the goal of extending and better developing the reservoir. The shallow geologic
Autor:
G. Bertini, Enrico Pandeli, Rinaldo Nicolich, Mariano Puxeddu, Ivano Dini, Fausto Batini, Giovanni Gianelli
Publikováno v:
Geothermics. 17:719-734
Geological, geophysical and petrologic data point to the presence of a granitic body below the geothermal region of Mt Amiata (central Italy). A broad area of about 900–1300 km 2 centered on Amiata volcano shows a regional uplift of the Pliocene be
Conference
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Conference
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