25 results on '"Corradino, Marta"'
Search Results
2. Resurgent uplift at large calderas and relationship to caldera-forming faults and the magma reservoir: New insights from the Neapolitan Yellow Tuff caldera (Italy)
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Corradino, Marta, Pepe, Fabrizio, Sacchi, Marco, Solaro, Giuseppe, Duarte, Henrique, Ferranti, Luigi, and Zinno, Ivana
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- 2021
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3. The holocene marine record of unrest, volcanism, and hydrothermal activity of Campi Flegrei and Somma–Vesuvius
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Sacchi, Marco, primary, Passaro, Salvatore, additional, Molisso, Flavia, additional, Matano, Fabio, additional, Steinmann, Lena, additional, Spiess, Volkhard, additional, Pepe, Fabrizio, additional, Corradino, Marta, additional, Caccavale, Mauro, additional, Tamburrino, Stella, additional, Esposito, Giuseppe, additional, Vallefuoco, Mattia, additional, and Ventura, Guido, additional
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- 2020
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4. Contributors
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Belkin, Harvey E., primary, Bodnar, Robert J., additional, Caccavale, Mauro, additional, Cannatelli, Claudia, additional, Carroll, Michael R., additional, Corradino, Marta, additional, Costanzo, Maria Rosaria, additional, Natale, Giuseppe De, additional, De Vivo, Benedetto, additional, Di Lascio, Massimo, additional, Esposito, Rosario, additional, Esposito, Giuseppe, additional, Fedele, Alessandro, additional, Fowler, Sarah Jane, additional, Gidwitz, Tom, additional, Kilburn, Christopher R.J., additional, Lima, Annamaria, additional, Macchiavelli, Chiara, additional, Matano, Fabio, additional, Milia, Alfonsa, additional, Molisso, Flavia, additional, Moretti, Roberto, additional, Nunziata, Concettina, additional, Panza, Giuliano Francesco, additional, Passaro, Salvatore, additional, Peccerillo, Angelo, additional, Penza, Giulia, additional, Pepe, Fabrizio, additional, Pierantoni, Pietro Paolo, additional, Rolandi, Giuseppe, additional, Rolandi, Roberto, additional, Ruberti, Daniela, additional, Sacchi, Marco, additional, Schettino, Antonio, additional, Somma, Renato, additional, Spera, Frank J., additional, Spiess, Volkhard, additional, Stabile, Paola, additional, Steinmann, Lena, additional, Tamburrino, Stella, additional, Torrente, Maurizio M., additional, Troise, Claudia, additional, Turco, Eugenio, additional, Vallefuoco, Mattia, additional, Ventura, Guido, additional, and Vigliotti, Marco, additional
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- 2020
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5. Boulder coastal deposits at Favignana Island rocky coast (Sicily, Italy): Litho-structural and hydrodynamic control
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Pepe, Fabrizio, Corradino, Marta, Parrino, Nicolò, Besio, Giovanni, Presti, Valeria Lo, Renda, Pietro, Calcagnile, Lucio, Quarta, Gianluca, Sulli, Attilio, and Antonioli, Fabrizio
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- 2018
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6. Arc and forearc rifting in the Tyrrhenian subduction system
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Corradino, Marta, primary, Balazs, Attila, additional, Faccenna, Claudio, additional, and Pepe, Fabrizio, additional
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- 2023
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7. Late Miocene to Recent Structural Evolution of the Squillace Gulf (Offshore Eastern Calabria): Insights on the Active Tectonics of the Calabrian Arc
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Corradino, Marta, primary, Morelli, Danilo, additional, Ceramicola, Silvia, additional, Scarfì, Luciano, additional, Barberi, Graziella, additional, Monaco, Carmelo, additional, and Pepe, Fabrizio, additional
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- 2022
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8. Synthesis and pharmacological characterization of a new series of 5,7-disubstituted-[1,2,4]triazolo[1,5-a][1,3,5]triazine derivatives as adenosine receptor antagonists: A preliminary inspection of ligand–receptor recognition process
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Pastorin, Giorgia, Federico, Stephanie, Paoletta, Silvia, Corradino, Marta, Cateni, Francesca, Cacciari, Barbara, Klotz, Karl-Norbert, Gao, Zhan-Guo, Jacobson, Kenneth A., Spalluto, Giampiero, and Moro, Stefano
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- 2010
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9. 16 - The holocene marine record of unrest, volcanism, and hydrothermal activity of Campi Flegrei and Somma–Vesuvius
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Sacchi, Marco, Passaro, Salvatore, Molisso, Flavia, Matano, Fabio, Steinmann, Lena, Spiess, Volkhard, Pepe, Fabrizio, Corradino, Marta, Caccavale, Mauro, Tamburrino, Stella, Esposito, Giuseppe, Vallefuoco, Mattia, and Ventura, Guido
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- 2020
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10. Resurgent uplift at large calderas and relationship to caldera-forming faults and the magma reservoir: new insights from the Neapolitan Yellow Tuff caldera (Italy)
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Corradino, Marta, primary, Pepe, Fabrizio, additional, Sacchi, Marco, additional, Solaro, Giuseppe, additional, Duarte, Henrique, additional, Ferranti, Luigi, additional, and Zinno, Ivana, additional
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- 2021
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11. Elusive active faults in a low strain rate region (Sicily, Italy): hints from a multidisciplinary land-to-sea approach
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Parrino, Nicolò, primary, Pepe, Fabrizio, additional, Burrato, Pierfrancesco, additional, Dardanelli, Gino, additional, Di Maggio, Cipriano, additional, Corradino, Marta, additional, and Pipitone, Claudia, additional
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- 2021
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12. 3D Architecture and Plio-Quaternary evolution of the Paola Basin: Insights into the Forearc of the Tyrrhenian-Ionian Subduction System
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Corradino, Marta, primary, Pepe, Fabrizio, additional, Bertotti, Giovanni, additional, Picotti, Vincenzo, additional, Monaco, Carmelo, additional, and Nicolich, Rinaldo, additional
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- 2020
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13. Active deformation evidence in the offshore of western Calabria (southern Tyrrhenian Sea) from ultra-resolution multichannel seismic reflection data: results from the Gulf of Sant'Eufemia
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Pepe, Fabrizio, primary, Kanari, Mor, additional, Burrato, Pierfrancesco, additional, Corradino, Marta, additional, Duarte, Henrique, additional, Ferranti, Luigi, additional, Monaco, Carmelo, additional, Sacchi, Marco, additional, and Tibor, Gideon, additional
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- 2020
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14. A roadmap for amphibious drilling at the Campi Flegrei caldera: insights from a MagellanPlus workshop
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Sacchi, Marco, primary, De Natale, Giuseppe, additional, Spiess, Volkhard, additional, Steinmann, Lena, additional, Acocella, Valerio, additional, Corradino, Marta, additional, de Silva, Shanaka, additional, Fedele, Alessandro, additional, Fedele, Lorenzo, additional, Geshi, Nobuo, additional, Kilburn, Christopher, additional, Insinga, Donatella, additional, Jurado, Maria-José, additional, Molisso, Flavia, additional, Petrosino, Paola, additional, Passaro, Salvatore, additional, Pepe, Fabrizio, additional, Porfido, Sabina, additional, Scarpati, Claudio, additional, Schmincke, Hans-Ulrich, additional, Somma, Renato, additional, Sumita, Mari, additional, Tamburrino, Stella, additional, Troise, Claudia, additional, Vallefuoco, Mattia, additional, and Ventura, Guido, additional
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- 2019
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15. The use and beauty of ultra-high-resolution seismic reflection imaging in Late Quaternary marine volcaniclastic settings, Napoli Bay, Italy
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Sacchi, Marco, primary, Caccavale, Mauro, additional, Corradino, Marta, additional, Esposito, Giuseppe, additional, Ferranti, Luigi, additional, Hámori, Zoltán, additional, Horváth †, Ferenc, additional, Insinga, Donatella, additional, Marino, Camilla, additional, Matano, Fabio, additional, Molisso, Flavia, additional, Natale, Jacopo, additional, Passaro, Salvatore, additional, Pepe, Fabrizio, additional, and Tóth, Tamás, additional
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- 2019
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16. A stalactite record of four relative sea-level highstands during the Middle Pleistocene Transition
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Stocchi, Paolo, Antonioli, Fabrizio, Montagna, Paolo, Pepe, Fabrizio, Lo Presti, Valeria, Caruso, Antonio, Corradino, Marta, Dardanelli, Gino, Renda, Pietro, Frank, Norbert, Douville, Eric, Thil, François, de Boer, Bas, Ruggieri, Rosario, Sciortino, Rosanna, Pierre, Catherine, Sub Dynamics Meteorology, Stratigraphy and paleontology, Marine and Atmospheric Research, Earth and Climate, Stocchi, P., Antonioli, F., Montagna, P., Pepe, F., Lo Presti, V., Caruso, A., Corradino, M., Dardanelli, G., Renda, P., Frank, N., Douville, E., Thil, F., de Boer, B., Ruggieri, R., Sciortino, R., Pierre, C., Royal Netherlands Institute for Sea Research (NIOZ), Utrecht University [Utrecht], Agenzia Nazionale per le nuove Tecnologie, l’energia e lo sviluppo economico sostenibile = Italian National Agency for New Technologies, Energy and Sustainable Economic Development (ENEA), Istituto di Science Marine (ISMAR ), National Research Council of Italy | Consiglio Nazionale delle Ricerche (CNR), Observatoire Astronomique de l'Université de Genève (ObsGE), Université de Genève = University of Geneva (UNIGE), Dipartimento di Scienze della Terra e del Mare [Palermo] (DiSTeM), Università degli studi di Palermo - University of Palermo, Universität Heidelberg [Heidelberg] = Heidelberg University, Géochrononologie Traceurs Archéométrie (GEOTRAC), Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] (LSCE), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS), Institute for Marine and Atmospheric Research [Utrecht] (IMAU), University of Nova Gorica, Biogéochimie-Traceurs-Paléoclimat (BTP), Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN), Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Sub Dynamics Meteorology, Stratigraphy and paleontology, Marine and Atmospheric Research, Agenzia Nazionale per le nuove Tecnologie, l’energia e lo sviluppo economico sostenibile (ENEA), Consiglio Nazionale delle Ricerche (CNR), Université de Genève (UNIGE), Universität Heidelberg [Heidelberg], Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Muséum national d'Histoire naturelle (MNHN)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS Paris), and Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Muséum national d'Histoire naturelle (MNHN)-Institut Pierre-Simon-Laplace (IPSL (FR_636))
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Marine isotope stage ,Archeology ,010504 meteorology & atmospheric sciences ,Settore GEO/02 - Geologia Stratigrafica E Sedimentologica ,Settore GEO/03 - Geologia Strutturale ,010502 geochemistry & geophysics ,01 natural sciences ,Sea level change ,Stable isotopes ,Global and Planetary Change ,geography.geographical_feature_category ,Ecology ,Archeology (arts and humanities) ,Geology ,87Sr/86Sr age ,Speleothem ,Stable isotope ,Pleistocene ,87Sr/86Sr ages ,Oceanography ,Archaeology ,[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology ,Sr/Sr ages ,Paleogeography ,Corals ,Stalactite ,Evolution ,Western Europe ,coastal ,87Sr/86 41 Sr ages ,Paleontology ,Interglacial(s) ,Behavior and Systematics ,14. Life underwater ,SDG 14 - Life Below Water ,[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces, environment ,Sea level ,Ecology, Evolution, Behavior and Systematics ,0105 earth and related environmental sciences ,U-Th dating ,geography ,Geomorphology ,Settore GEO/01 - Paleontologia E Paleoecologia ,Karst ,Ecology, Evolution, Behavior and Systematic ,Speleothems ,Sea level changes ,Coral ,Quaternary ,Settore ICAR/06 - Topografia E Cartografia - Abstract
International audience; Ice-sheet and sea-level fluctuations during the Early and Middle Pleistocene are as yet poorly understood. A stalactite from a karst cave in North West Sicily (Italy) provides the first evidence of four marine inundations that correspond to relative sea-level highstands at the time of the Middle Pleistocene Transition. The speleothem is located ∼97 m above mean sea level as result of Quaternary uplift. Its section reveals three marine hiatuses and a coral overgrowth that fixes the age of final marine ingression at 1.124 ± 0.2, thus making this speleothem the oldest stalactite with marine hiatuses ever studied to date. Scleractinian coral species witness light-limited conditions and water depth of 20–50 m. Integrating the coral-constrained depth with the geologically constrained uplift rate and an ensemble of RSL scenarios, we find that the age of the last marine ingression most likely coincides with Marine Isotope Stage 35 on the basis of a probabilistic assessment. Our findings are consistent with a significant Antarctic ice-sheet retreat.
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- 2017
17. Fore-arc Deformation in the Paola Basin Segment (Offshore Western Calabria) of the Tyrrhenian‐Ionian Subduction System
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Pepe Fabrizio, Corradino Marta, Nicolich Rinaldo, Barreca Giovanni, Bertotti Giovanni, Ferranti Luigi, Monaco Carmelo, Pepe, F., Corradino, M., Nicolich, R., Barreca, G., Bertotti, G., Ferranti, L., and Monaco, C.
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Fore-arc basin ,Settore GEO/02 - Geologia Stratigrafica E Sedimentologica ,Southern Tyrrhenian Sea ,Settore GEO/03 - Geologia Strutturale ,Calabrian Arc - Abstract
The 3D stratigraphic architecture and Late Neogene to Recent tectonic evolution of the Paola Basin (offshore western Calabria), a segment in the fore-arc of the Tyrrhenian‐Ionian subduction system, is reconstructed by using a grid of high-penetration reflection seismics. Oligocene to Messinian deposits are interpreted all along the profile. They tend to fossilize preexisting topography and reach the largest thicknesses between (fault controlled) basement highs. Plio‐ Quaternary deposits are found over the entire area and display variations in thickness and tectonic style. They are thicken up to 4.5 km in the depocenter of the basin, and decrease both in the east and west termination of the lines. The Paola Basin can be partitioned into two sectors with different tectonic deformation, separated by a NNW-SSE elongated area that coincides with the basin depocenter. Tectonic features associated with strike-slip restraining and releasing bends are widely spread over the western sector of the basin. Overall, they form an approximately NStrending and geomorphically prominent ridge separating the Paola Basin from the Marsili abyssal plain. A high-angle, NNE-trending, normal fault system develops on the south-west tip of the basin, where the faults offset the Messinian horizon of ca. 500 m. Data suggest that limited vertical slip occurs along reverse faults detected at the border and inside the sedimentary infilling of the Paola Basin, reaching thickness of more than 3.8s two way travel time. The reflection sequence pattern can be interpreted as a result of the infilling of the thrust-top basin related to a prograding system, located between a growth ramp-anticline to the west and a culmination of basement-thrust sheets to the East. We propose that the Paola Basin developed near the northern edge of the Ionian slab where tearing of the lithosphere is expected. Also, the strike-slip fault system is a kinematic consequence of obliquely convergent subduction settings, where interplate strain is partitioned into arc-parallel strike-slip zones within the fore-arc, arc or back-arc region.
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- 2017
18. Active Tectonics along the South East Offshore Margin of Mt. Etna: New Insights from High-Resolution Seismic Profiles
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Barreca, Giovanni, primary, Corradino, Marta, additional, Monaco, Carmelo, additional, and Pepe, Fabrizio, additional
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- 2018
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19. Architecture and kinematics of forearc basins and intra-caldera resurgences: new insight from the Paola Basin (western offshore Calabria region) and the Campi Flegrei caldera (Campania region)
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Corradino, Marta, PEPE, Fabrizio, and AIUPPA, Alessandro
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Settore GEO/03 - Geologia Strutturale ,Caldera, Resurgence, Reverse faults, Campi Flegrei, Pozzuoli Bay ,Calabrian Arc, Ionian Sea, Fore-arc basin, Lithospheric buckling, Longshore current - Abstract
This thesis deals with the patterns of tectonic deformation at different time and spatial scales ranging from tens to millions of years and from one to tens of kilometers, respectively. The study areas are the Campi Flegrei (Campania region, Italy) and Paola Basin (western offshore Calabria region, Italy). The Campi Flegrei and its offshore prolongation, the Pozzuoli Bay, are a laboratory for investigating volcano-tectonic deformations at 1yr-1kyr timescale and 1km spatial scale related to the dynamics of the Neapolitan Yellow Tuff (NYT) caldera and its intra-caldera resurgence. Resurgence is the late stage, long-term uplift of a collapse caldera floor to form a dome-like structure. The comprehension of its development and structural pattern is crucial for predicting the caldera behaviour during periods of unrest. This work investigates the resurgent activity of the NYT caldera using an integrated analysis of high-resolution swath bathymetry, reflection seismic profiles and interferometric synthetic-aperture radar (InSAR) data. The interpretation of the data shows that resurgence affects a ~ 50 km2 wide almost circular area centred in the Pozzuoli harbor. The resurgent area is surrounded by a ~ 3-4 km wide structural discontinuity corresponding to the Ring Fault Zone (RFZ) that formed during the NYT caldera collapse (~15 ka BP). The uplift of the caldera resurgence occurs along a series of inward-dipping reverse faults of the RFZ characterized by a decreasing-upward inclination of fault planes from ~70° to ~15°. The development of these structures is controlled by the reactivation and deformation of pre-exiting normal faults associated with the NYT caldera collapse. Deformation of reactivated faults often results in folding of overlying and/or juxtaposed strata, in the style of ~ 500 m wide antiformal folds, mostly located along the periphery of the resurgent area. The structural pattern of the resurgence consists of disjoint uplifted blocks of the caldera floor. Two main structural elements are detected inside the resurgent area both off- and onshore, separated by a NNE-SSW trending high-angle normal fault. The most uplifted block comprises the area from Mt Nuovo to La Pietra, whereas the adjacent uplifted sector extends eastwards to include Mt Spina. The morpho-bathymetric expression of the two uplifted blocks is represented by a ~5 km wide antiformal structure, encircled by Bagnoli and Epitaffio valleys. In the hinge zone of the resurgent dome a series of high-angle normal faults form a small apical graben. In order to analyze long term deformations (Myr timescale) occurring at a tens of kilometers spatial scale, this study focuses on the Paola Basin, a segment of the forearc region of the Tyrrhenian-Ionian subduction system. Fore-arc basins are parts of fore-arc region that form structurally in response to a variety of subduction zone processes. The sedimentary infill records the complex tectono-stratigraphic evolution of basin associated with subduction system, and thus, allows deciphering the formation mechanisms of basins developed in compressional intraplate settings. We analyse these processes in the Paola Basin using reflection seismic profiles and bathymetric data. The Paola Basin is a NNW-SSE trending asymmetric syncline, bounded by the offshore sector of the Coastal Chain to the East and by the regional-scale Paola Anticline to the West. It hosts up to 5.5 km thick Plio-Quaternary deposits, most of them showing eastward-dipping clinoforms. These latter are associated to shelfal progradation, supplied from the north via longshore currents, dispersing sediments from unknown Apenninic/Sila entry points. A local circulation of longshore currents flowed southwards and dispersed sediments from unknown Apenninic/Sila entry points. An aggradational internal geometry characterizes the uppermost part of the sedimentary infill with a thickness decreasing westwards, suggesting a sediment supply from the Coastal Chain. In the Early Pliocene, the proto Paola Basin extended from the Paola Anticline up to the western flank of the Sila Massif. Since ∼ 3.5 Ma, the uplift of the Coastal Chain shortened the proto Paola Basin, leading to the separation of the basin from the Crati basin. Short wavelength (∼ 80 km) lithospheric buckling, caused by a ENE-WSW oriented, arc-normal paleo-stress field, is the most likely mechanism that explains the pattern of tectonic subsidence of the Paola Basin, the uplift of the Paola Anticline and part of the uplift experienced by Sila Massif during the Plio-Quaternary. Kilometre-scale, strike-slip restraining and releasing bends are widely spread over the hinge zone of the Paola Anticline, defining the Paola Ridge. Their formation is compatible with an NW-SE oriented maximum stress axis meanwhile strike-slip fault accommodates the arc-parallel component of the plate motion. The change in direction from ENE-WSW to NW-SE of the maximum stress axis in the fore-arc region is a consequence of the transition from orthogonal to oblique subduction, associated to the bending of the Northern Calabria Arc. Regional uplift and folding of the Northern Calabrian Arc induced tensile stress resulting in the formation of N-S trending normal faults in the extrados of the Sila Massif anticline. In this context, the Paola Basin can be defined as a “Neutral Accretionary-type” forearc basin.
20. Synthesis and pharmacological characterization of a new series of 5,7-disubstituted-[1,2,4]triazolo[1,5-a][1,3,5]triazine derivatives as adenosine receptor antagonists: a preliminary receptor-driven SAR profile
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Pastorin, Giorgia, Stephanie Federico, Cateni, Francesca, Cacciari, Barbara, Klotz, Karl-Norbert, Gao, Zhan-Guo, Jacobson, Kenneth A., Corradino, Marta, Paoletta, Silvia, Moro, Stefano, and Spalluto, Giampiero
21. Active deformation evidence in the offshore of western Calabria (southern Tyrrhenian Sea) from ultra-resolution multichannel seismic reflection data: results from the Gulf of Sant'Eufemia
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Fabrizio Pepe, Mor Kanari, Pierfrancesco Burrato, Marta Corradino, Henrique Duarte, Luigi Ferranti, Carmelo Monaco, Marco Sacchi, Gideon Tibor, Pepe, Fabrizio, Kanari, Mor, Burrato, Pierfrancesco, Corradino, Marta, Duarte, Henrique, Ferranti, Luigi, Monaco, Carmelo, Sacchi, Marco, and Tibor, Gideon
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Active tectonics, Calabrian Arc - Abstract
An ultra-resolution, multichannel seismic reflection data set was collected during an oceanographic cruise organised in the frame of the “Earthquake Potential of Active Faults using offshore Geological and Morphological Indicators” (EPAF) project, which was founded by the Scientific and Technological Cooperation (Scientific Track 2017) between the Italian Ministry of Foreign Affairs and International Cooperation and the Ministry of Science, Technology and Space of the State of Israel. The data acquisition approach was based on innovative technologies for the offshore imaging of stratigraphy and structures along continental margins with a horizontal and vertical resolution at decimetric scale. In this work, we present the methodology used for the 2D HR-seismic reflection data acquisition and the preliminary interpretation of the data set. The 2D seismic data were acquired onboard the R/V Atlante by using an innovative data acquisition equipment composed by a dual-sources Sparker system and one HR 48-channel, slant streamers, with group spacing variable from 1 to 2 meters, at 10 kHz sampling rate. An innovative navigation system was used to perform all necessary computations to determining real-time positions of sources and receivers. The resolution of the seismic profiles obtained from this experiment is remarkable high respect to previously acquired seismic data for both scientific and industrial purposes. In addition to the seismic imaging, gravity core data were also collected for sedimentological analysis and to give a chronological constraint using radiocarbon datings to the shallower reflectors. The investigated area is located in the western offshore sector of the Calabrian Arc (southern Tyrrhenian Sea) where previous research works, based on multichannel seismic profiles coupled with Chirp profiles, have documented the presence of an active fault system. One of the identified faults was tentatively considered as the source of the Mw 7, 8 September 1905 seismic event that hit with highest macroseismic intensities the western part of central Calabria, and was followed by a tsunami that inundated the coastline between Capo Vaticano and the Angitola plain. On this basis, the earthquake was considered to have a source at sea, but so far, the location, geometry and kinematics of the causative fault are still poorly understood. In this study we provide preliminary results of the most technologically advanced ultra-high-resolution geophysical method used to reveal the 3D faulting pattern, the late Quaternary slip rate and the earthquake potential of the marine fault system located close to the densely populated west coast of Calabria.
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- 2020
22. A roadmap for amphibious drilling at the Campi Flegrei caldera: insights from a MagellanPlus workshop
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Marco Sacchi1, Giuseppe De Natale2, Volkhard Spiess3, Lena Steinmann3, Valerio Acocella4, Marta Corradino5, Shanaka de Silva6, Alessandro Fedele2, Lorenzo Fedele7, Nobuo Geshi8, Christopher Kilburn9, Donatella Insinga1, Maria-José Jurado10, Flavia Molisso1, Paola Petrosino7, Salvatore Passaro1, Fabrizio Pepe5, Sabina Porfido11, 2, Claudio Scarpati7, Hans-Ulrich Schmincke12, Renato Somma2, Mari Sumita12, Stella Tamburrino1, Claudia Troise2, Mattia Vallefuoco1, and Guido Ventura13, European Consortium for Ocean Research Drilling, Jurado, Maria José [0000-0001-8165-2729], Sacchi M., De Natale G., Spiess V., Steinmann L., Acocella V., Corradino M., De Silva S., Fedele A., Fedele L., Geshi N., Kilburn C., Insinga D., Jurado M.-J., Molisso F., Petrosino P., Passaro S., Pepe F., Porfido S., Scarpati C., Schmincke H.-U., Somma R., Sumita M., Tamburrino S., Troise C., Vallefuoco M., Ventura G., Sacchi, M., De Natale, G., Spiess, V., Steinmann, L., Acocella, V., Corradino, M., de Silva, S., Fedele, A., Fedele, L., Geshi, N., Kilburn, C., Insinga, D., Jurado, M. J., Molisso, F., Petrosino, P., Passaro, S., Pepe, F., Porfido, S., Scarpati, C., Schmincke, H. U., Somma, R., Sumita, M., Tamburrino, S., Troise, C., Vallefuoco, M., Ventura, G., Sacchi, Marco, De Natale, Giuseppe, Spiess, Volkhard, Steinmann, Lena, Acocella, Valerio, Corradino, Marta, de Silva, Shanaka, Fedele, Alessandro, Fedele, Lorenzo, Geshi, Nobuo, Kilburn, Christopher, Insinga, Donatella, Jurado, Maria-José, Molisso, Flavia, Petrosino, Paola, Passaro, Salvatore, Pepe, Fabrizio, Porfido, Sabina, Scarpati, Claudio, Schmincke, Hans-Ulrich, Somma, Renato, Sumita, Mari, Tamburrino, Stella, Troise, Claudia, Vallefuoco, Mattia, Ventura, Guido, and Jurado, Maria José
- Subjects
010504 meteorology & atmospheric sciences ,Calderas ,Geochemistry ,Energy Engineering and Power Technology ,Pyroclastic rock ,Volcanology ,Magma chamber ,Volcanism ,010502 geochemistry & geophysics ,01 natural sciences ,drilling ,southern Italy ,caldera ,Caldera ,14. Life underwater ,0105 earth and related environmental sciences ,geography ,geography.geographical_feature_category ,Mechanical Engineering ,lcsh:QE1-996.5 ,MagellanPlus workshop ,International Ocean Discovery Program ,lcsh:Geology ,Campi Flegrei caldera ,Volcano ,Italy ,13. Climate action ,Eruption ,Magma ,caldera, Campi Flegrei, monitopring system, hydrothermal system, IODP ,Campi Flegrei ,Geology - Abstract
Large calderas are among the Earth's major volcanic features. They are associated with large magma reservoirs and elevated geothermal gradients. Caldera-forming eruptions result from the withdrawal and collapse of the magma chambers and produce large-volume pyroclastic deposits and later-stage deformation related to post-caldera resurgence and volcanism. Unrest episodes are not always followed by an eruption; however, every eruption is preceded by unrest. The Campi Flegrei caldera (CFc), located along the eastern Tyrrhenian coastline in southern Italy, is close to the densely populated area of Naples. It is one of the most dangerous volcanoes on Earth and represents a key example of an active, resurgent caldera. It has been traditionally interpreted as a nested caldera formed by collapses during the 100–200 km3 Campanian Ignimbrite (CI) eruption at ∼39 ka and the 40 km3 eruption of the Neapolitan Yellow Tuff (NYT) at ∼15 ka. Recent studies have suggested that the CI may instead have been fed by a fissure eruption from the Campanian Plain, north of Campi Flegrei. A MagellanPlus workshop was held in Naples, Italy, on 25–28 February 2017 to explore the potential of the CFc as target for an amphibious drilling project within the International Ocean Discovery Program (IODP) and the International Continental Drilling Program (ICDP). It was agreed that Campi Flegrei is an ideal site to investigate the mechanisms of caldera formation and associated post-caldera dynamics and to analyze the still poorly understood interplay between hydrothermal and magmatic processes. A coordinated onshore–offshore drilling strategy has been developed to reconstruct the structure and evolution of Campi Flegrei and to investigate volcanic precursors by examining (a) the succession of volcanic and hydrothermal products and related processes, (b) the inner structure of the caldera resurgence, (c) the physical, chemical, and biological characteristics of the hydrothermal system and offshore sediments, and (d) the geological expression of the phreatic and hydromagmatic eruptions, hydrothermal degassing, sedimentary structures, and other records of these phenomena. The deployment of a multiparametric in situ monitoring system at depth will enable near-real-time tracking of changes in the magma reservoir and hydrothermal system., This research has been supported by the European Consortium for Ocean Research Drilling (ECORD) through the ECORD/ICDP MagellanPlus Workshop Series Programme (grant no. 2017.2376/4/AF).
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- 2019
23. The use and beauty of ultra-high-resolution seismic reflection imaging in Late Quaternary marine volcaniclastic settings, Napoli Bay, Italy
- Author
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Giuseppe Esposito, Flavia Molisso, M. Corradino, Jacopo Natale, Donatella Insinga, Salvatore Passaro, Zoltán Hámori, Luigi Ferranti, Ferenc Horváth, Marco Sacchi, Mauro Caccavale, Fabrizio Pepe, Tamás Tóth, Camilla Marino, Fabio Matano, Sacchi, Marco, Caccavale, Mauro, Corradino, Marta, Esposito, Giuseppe, Ferranti, Luigi, Hámori, Zoltán, Horváth †, Ferenc, Insinga, Donatella Domenica, Marino, Camilla, Matano, Fabio, Molisso, Flavia, Natale, Jacopo, Passaro, Salvatore, Pepe, Fabrizio, Tóth, Tamás, and Insinga, Donatella
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Settore GEO/02 - Geologia Stratigrafica E Sedimentologica ,Settore GEO/03 - Geologia Strutturale ,Stratigraphy ,Volcaniclastic settings ,Pyroclastic rock ,Fault (geology) ,Paleontology ,Geochemistry and Petrology ,Pumice ,Campania Volcanism ,Stratovolcano ,Somma-Vesuvius ,high-resolution single channel reflection seismics, Campania Volcanism, Volcaniclastic settings, Campi Flegrei, Caldera ring fault, Somma-Vesuvius, Late Quaternary, Bay of Naples ,geography ,geography.geographical_feature_category ,Continental shelf ,Resurgent dome ,Caldera ring fault ,Geology ,Late Quaternary ,Seafloor spreading ,Volcano ,High-resolution single channel reflection seismics ,Bay of Naples ,Campi Flegrei - Abstract
A Nápolyi-öbölben felvett ultra nagy felbontású egycsatornás (IKB-Seistec™) reflexiós szeizmikus szelvények korábbi geológiai és geofizikai vizsgálatok eredményeivel együtt kivételes, eddig soha nem látott felbontású szeizmikus leképezését nyújtják a Flegrei-mezők és a Somma-Vezúv felszín alá süllyedt késő-pleisztocén–holocén rétegtani felépí - tésének. A szeizmikus szelvényeken látott geometria és gravitációs magvevővel nyert üledékek adatainak összevetéséből Campania partközeli kontinentális talapzatán számos olyan üledékes és vulkáni szerkezet, valamint hidrotermális jelenség került leképezésre, melyek a legutolsó glaciális maximum (kb. 18 000 év) óta keletkeztek. A Pozzuoli-öbölben mért Seistec szelvények jól mutatják a beomlott kaldera gyűrűs vetőjét, a kb. 15 ezer éves Nápolyi Sárga Tufa (NYT) lerakódáshoz vezető kitöréskor felújuló boltozatot, és alátámasztják a deformáció későnegyedidőszaki korára és stílusára vonatkozó hipotéziseket. A szeizmikus szelvényeken látható a NYT rétegeinek töréses szerkezete, valamint hidrotermális fluidum-feláramlások és vulkáni/szubvulkáni intrúziók a gyűrűs vetők mentén. A Somma-Vezúv rétegvulkán előterében a kontinentális talapzat felett mért szeizmikus szelvények leképezték a Vezúv i.sz. 79-es kitörésekor Herculaneum városát elpusztító piroklaszt-ár tengervízbe érésekor keletkező, gravitációsan összeomló homokhullámok szerkezetét is. A Somma-Vezúv és a Pozzuoli-öböl közti, buckás felszínű Banco della Montagna területén mért szelvények és fúrómagok vulkanoklasztos diapírok sorát tárták fel. Ezeket a konszolidálatlan horzsakőből álló testeket a fluidum - feláramlás és aktív kigázosodás hatására kialakult mélybeli túlnyomás hozta fel a tengerfenékre. Very high-resolution, single channel (IKB-Seistec™) reflection seizmic profiles acquired in the Bay of Naples, com - plemented with geological and geophysical data from the literature, provide unprecedented, superb seismic imaging of the latest Pleistocene–Holocene stratigraphic architecture of the submerged sectors Campi Flegrei and Somma-Vesuvius volcanic districts. Seismic profiles were calibrated by gravity core data and document a range of depositional systems, volcanic structures and hydrothermal features that evolved after the onset of the Last Glacial Maximum (~ 18 ka BP) over the continental shelf on the Campania coastal zone. Seistec profiles from the Pozzuoli Bay yield high-resolution images of the shallow structure of the collapse caldera-ring fault — resurgent dome system associated with the eruption of the Neapolitan Yellow Tuff (NYT) (ca 15 ka) and support a working hypothesis to assess the timing and the styles of deformation of the NYT resurgent structure throughout the latest Quaternary. Seismic images also revealed the nature of the fragile deformation of strata along the NYT ring fault system and the occurrence of hydrothermal fluids and volcanic/subvolcanic intrusions ascending along the ring fault zone. Seismic data acquired over the continental shelf off the Somma-Vesuvius stratovolcano, display evidence of gravit - ational instability of wavy bedforms representing the submarine prosecution of pyroclastic flows originated from the Vesuvius during the eruption that destroyed the Roman city of Herculaneum in 79 CE. At the Banco della Montagna, a hummocky seafloor knoll located between the Somma-Vesuvius and the Pozzuoli Bay, seismic profiles and gravity core data revealed the occurrence of a field of volcaniclastic diapirs formed by the dragging and rising up of unconsolidated pumice, as a consequence of fluid overpressure at depth associated with active degassing and fluid venting at the seafloor.
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- 2019
24. Active tectonics along the south east offshore margin of Mt. Etna: New insights from high-resolution seismic profiles
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Giovanni Barreca, Fabrizio Pepe, Carmelo Monaco, M. Corradino, Barreca, Giovanni, Corradino, Marta, Monaco, Carmelo, and Pepe, Fabrizio
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010504 meteorology & atmospheric sciences ,Pleistocene ,Settore GEO/02 - Geologia Stratigrafica E Sedimentologica ,Settore GEO/03 - Geologia Strutturale ,active tectonics ,010502 geochemistry & geophysics ,01 natural sciences ,Sicilian thrust-belt ,Paleontology ,Active tectonic ,Active tectonics ,Ionian Sea ,Mt. Etna ,Seismic investigation ,Earth and Planetary Sciences (all) ,Holocene ,0105 earth and related environmental sciences ,geography ,geography.geographical_feature_category ,Continental shelf ,lcsh:QE1-996.5 ,Fold (geology) ,seismic investigation ,Seafloor spreading ,Volcanic rock ,lcsh:Geology ,Tectonics ,General Earth and Planetary Sciences ,Sedimentary rock ,Geology - Abstract
The offshore margin of Mt. Etna has been shaped by Middle Pleistocene to Holocene shortening and extension and, more recently, by gravity-related sliding of the volcanic edifice. These processes have acted contemporaneously although the gravitational component largely prevails over the tectonic one. In order to investigate this issue, we focused on the main role of active tectonics along the south-eastern offshore of Mt. Etna by means of marine high-resolution seismic data. Seismic profiles revealed post-220 ka sedimentary deposits unconformably overlaying the Lower-Middle Pleistocene Etnean clayey substratum and volcanics of the Basal Tholeiitic phase and the Timpe phase. Offshore Aci Trezza-Catania, the architecture of the sedimentary deposits reflects syn-tectonic deposition occurred into âpiggy-backâ basin setting. Shortening rate was estimated at ~0.5 mm/a since ~220 ka. Asymmetric folding also involves post Last Glacial Maximum deposits, evidencing that compressional deformation is still active. In the continental slope, a belt of normal faults offset the Lower-Middle Pleistocene Etnean clayey substratum and younger deposits, also producing seafloor ruptures. Thrust and fold structures can be related to the recent migration of the Sicilian chain front, while extensional faults are interpreted as part of a major tectonic boundary located in the Ionian offshore of Sicily.
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- 2018
25. Boulder coastal deposits at Favignana Island rocky coast (Sicily, Italy): Litho-structural and hydrodynamic control
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Fabrizio Pepe, Giovanni Besio, Gianluca Quarta, M. Corradino, Nicolò Parrino, Valeria Lo Presti, Lucio Calcagnile, Fabrizio Antonioli, P. Renda, Attilio Sulli, Pepe, Fabrizio, Corradino, Marta, Parrino, Nicolò, Besio, Giovanni, Presti, Valeria Lo, Renda, Pietro, Calcagnile, Lucio, Quarta, Gianluca, Sulli, Attilio, Antonioli, Fabrizio, Pepe, F., Corradino, M., Parrino, N., Besio, G., Valeria Lo, P., Renda, P., Calcagnile, L., Quarta, G., Sulli, A., Antonioli, F., and Presti, V. L.
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010504 meteorology & atmospheric sciences ,Bedding ,Settore GEO/02 - Geologia Stratigrafica E Sedimentologica ,Lithology ,Carbonate platform ,Settore GEO/03 - Geologia Strutturale ,Storm wave ,010502 geochemistry & geophysics ,01 natural sciences ,Hydrodynamic equations ,Boulders ,Fracture network ,Storm waves ,Earth-Surface Processes ,Bed ,Geomorphology ,Boulder ,0105 earth and related environmental sciences ,Boulders,.Fracture network, Hydrodynamic, equations, Storm waves ,Berm ,Storm ,Hydrodynamic equation ,Clastic rock ,Fracture (geology) ,Geology - Abstract
Boulders are frequently dislodged from rock platforms, transported and deposited along coastal zones by high-magnitude storm waves or tsunamis. Their size and shape are often controlled by the thickness of bedding planes as well as by high-angle to bedding fracture network. We investigate these processes along two coastal areas of Favignana Island by integrating geological data for 81 boulders, 49 rupture surfaces (called sockets) and fracture orientation and spacing with four radiocarbon dates, numerical hydrodynamic analysis, and hindcast numerical simulation data. Boulders are scattered along the carbonate platform as isolated blocks or in small groups, which form, as a whole, a discontinuous berm. Underwater surveys also highlight free boulders with sharp edges and sockets carved out in the rock platform. Boulders are composed of ruditic- to arenitic-size clastic carbonates. Their size ranges from 0.6 to 3.7 m, 0.55 to 2.4 m, and 0.2 to 1 m on the major (A), medium (B), and minor (C) axes, respectively. The highest value of mass estimation is 12.5 t. Almost all of boulders and sockets are characterized by a tabular or bladed shape. The comparisons between a) the fractures spacing and the length of A- and B-axes, and b) the frequency peaks of C-axis with the recurrent thickness of beds measured along the coastal zone demonstrate the litho-structural control in the size and shape of joint-bounded boulders. These comparisons, together with the similarity between the shapes of the boulders and those of the sockets as well as between the lithology of boulders and the areas surrounding the sockets, suggest that blocks originate by detachment from the platform edge. Thus, the most common pre-transport setting is the joint-bounded scenario. Hydrodynamic equations estimate that the storm wave heights necessary to initiate the transport of blocks diverge from ~ 2 m to ~ 8 m for joint-bounded boulders and from few tens of centimeters up to ~ 11 m for submerged boulders. The comparison between the wave heights at the breaking point of the coastal zones with the results of hydrodynamic equations shows that waves approaching the coastline are able to transport all surveyed boulders. Our data suggest that boulders have been transported by several storm events, even in very recent times. © 2017 Elsevier B.V.
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- 2018
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