Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Francesco Fanucci"'
Autor:
Umberta Tinivella, Maria Filomena Loreto, Francesco Fanucci, Iván Vargas-Cordero, Flavio Accaino
Publikováno v:
Marine and Petroleum Geology. 27:1148-1156
In the last decades gas hydrate occurrence along the Chilean continental margin has been well documented. In order to better define the seismic character of the hydrate-bearing sediments, we performed a detailed velocity analysis by using the pre-sta
Autor:
Ivan de la Cruz Vargas Cordero, Flavio Accaino, Maria Filomena Loreto, Umberta Tinivella, Christian Reichert, Francesco Fanucci
Publikováno v:
Geo-Marine Letters. 30:271-281
Two seismic sections offshore Arauco and Coyhaique, Chile, have been analysed to better define the seismic character of hydrate-bearing sediments. The velocity analysis was used to estimate the gas-phase concentration, which can serve to correlate hy
Publikováno v:
Chemistry and Ecology. 22:S349-S359
The Ligurian continental shelf is a terrigenous platform characterized by variable extension and subsidence of the continental margin and thick accumulation of sediments originated by repeated sea-level oscillations. Its genesis and evolution occurre
Autor:
Martina Busetti, Silvia Ceramicola, Silvana D'Angelo, Rinalda Di Stefano, Francesco Fanucci, Andrea Fiorentino, Maria Filomena Loreto, Danilo Morelli e Valentina Volpi
Publikováno v:
AIQUA,, Napoli (Italy)., 15-21/02/2013
info:cnr-pdr/source/autori:Martina Busetti, Silvia Ceramicola, Silvana D'Angelo, Rinalda Di Stefano, Francesco Fanucci, Andrea Fiorentino, Maria Filomena Loreto, Danilo Morelli e Valentina Volpi/congresso_nome:AIQUA,/congresso_luogo:Napoli (Italy)./congresso_data:15-21%2F02%2F2013/anno:2013/pagina_da:/pagina_a:/intervallo_pagine
info:cnr-pdr/source/autori:Martina Busetti, Silvia Ceramicola, Silvana D'Angelo, Rinalda Di Stefano, Francesco Fanucci, Andrea Fiorentino, Maria Filomena Loreto, Danilo Morelli e Valentina Volpi/congresso_nome:AIQUA,/congresso_luogo:Napoli (Italy)./congresso_data:15-21%2F02%2F2013/anno:2013/pagina_da:/pagina_a:/intervallo_pagine
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::95bd6031b3f8a514af153249ef99c6f8
https://publications.cnr.it/doc/294261
https://publications.cnr.it/doc/294261
The aim of this work is to describe the morpho-dynamic processes of coastal and submarine areas based on morpho-bathymetric data and sub-bottom acoustic profiles from the Calabrian Ionian margin (from Capo Spartivento to Capo Rizzuto). We describe so
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::097d61363b9694a10c3cef8efbb4532f
https://hdl.handle.net/11368/2604021
https://hdl.handle.net/11368/2604021
Autor:
Francesco Fanucci
Publikováno v:
Zeitschrift für Geomorphologie. 31:463-472
Publikováno v:
Marine Geology. 55:291-303
A map of the thickness of Plio-Quaternary sediments in the Ligurian Sea is presented here, made from the data of seismic reflection methods, collected by the “Istituto di Geologia” of Genoa and the “Istituto di Oceanologia” of Naples. An expl
Autor:
Christian Reichert, Umberta Tinivella, Maria Filomena Loreto, Flavio Accaino, I. Vargas Cordero, Francesco Fanucci
Publikováno v:
Scopus-Elsevier
We used a procedure already tested in order to characterize the gas hydrate and free gas reservoir along South Chile. We used the multichannel seismic data to obtain an accurate velocity model by using the Pre stack Depth Migration. The velocity mode
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b03dce614a3ba3f9f72790bca729249b
http://www.scopus.com/inward/record.url?eid=2-s2.0-77649295286&partnerID=MN8TOARS
http://www.scopus.com/inward/record.url?eid=2-s2.0-77649295286&partnerID=MN8TOARS
Autor:
I. Vargas Cordero, Maria Filomena Loreto, Flavio Accaino, Francesco Fanucci, M. E. Lascano, Christian Reichert, Umberta Tinivella
Publikováno v:
Scopus-Elsevier
From seismic interpretation we can argue that basal and frontal accretions are the main processes that model this part of the Chilean margin. Frontal accretion areas are characterized by a smoothed oceanic crust top, anticline reliefs, high offset th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fde63188fb8203a56e2ad1bd929ebeaf
http://www.scopus.com/inward/record.url?eid=2-s2.0-84898941696&partnerID=MN8TOARS
http://www.scopus.com/inward/record.url?eid=2-s2.0-84898941696&partnerID=MN8TOARS