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Mauro Rosi - One of the best experts on this subject based on the ideXlab platform.
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Eruptions of the last 2200 years at Vulcano and Vulcanello (Aeolian Islands, Italy) dated by high-accuracy archeomagnetism
Physics of the Earth and Planetary Interiors, 2006Co-Authors: Simone Arrighi, Jean-claude Tanguy, Mauro RosiAbstract:The recent eruptive history of the Vulcano island (Southern Italy) was investigated through the high-accuracy “large sample” archeomagnetic method (Tanguy, J.C., Le Goff, M., Principe, C., Arrighi, S., Chillemi, V., Paiotti, A., La Delfa, S., Patane, G., 2003. Archeomagnetic dating of Mediterranean volcanics of the last 2100 years: validity and limits. Earth Planet. Sci. Lett. 211, 111–124; Tanguy, J.C., Principe, C., Arrighi, S., 2005. Comment on “Historical measurements of the Earth's magnetic field compared with remanence directions from lava flows in Italy over the last four centuries” by R. Lanza, A. Meloni, and E. Tema. Phys. Earth Planet. Interiors 152, 116–120; Arrighi, S., 2004. The large sample archeomagnetic method applied to Neapolitan volcanoes and Aeolian Islands. PhD Thesis. University of Pisa, Italy, pp. 1–186). Age determination is based upon directional geomagnetic variation reconstructed from historically dated lavas in Southern Italy, and from archeological sites in Western Europe (Gallet, Y., Genevey, A., Le Goff, M., 2002. Three millennia of directional variation of the Earth's magnetic field in Western Europe as revealed by archeological artefacts. Phys. Earth Planet. Interiors 131, 81–89) relocated to Sicily. Results in the present paper were obtained on 12 sites including 185 samples weighing 0.5–1 kg, distributed over the Vulcanello platform lavas and pyroclastic cones, and on the lava flows from the Fossa cone. It is shown that the Vulcanello platform was built by nearly continuous activity between AD 1000 and 1250, which is more than a millennium younger than believed until now from questionable interpretation of imprecise historical accounts. Most of the lavas from the Fossa cone, whose ages were rather hypothetical or known with a large uncertainty, have erupted within the same period. However, the last “Pietre Cotte” obsidian flow is confirmed to date from 1720 ± 30, in agreement with historical data (1739).
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Eruptions of the last 2200 years at Vulcano and Vulcanello (Aeolian Islands, Italy) dated by high-accuracy archeomagnetism
Physics of the Earth and Planetary Interiors, 2006Co-Authors: Simone Arrighi, J-Y Tanguy, Mauro RosiAbstract:The recent eruptive history of the Vulcano island (Southern Italy) was investigated through the high-accuracy "large sample" archeomagnetic method (Tanguy, J.C., Le Goff, M., Principe, C., Arrighi, S., Chillemi, V., Paiotti, A., La Delfa, S., Patan??, G., 2003. Archeomagnetic dating of Mediterranean volcanics of the last 2100 years: validity and limits. Earth Planet. Sci. Lett. 211, 111-124; Tanguy, J.C., Principe, C., Arrighi, S., 2005. Comment on "Historical measurements of the Earth's magnetic field compared with remanence directions from lava flows in Italy over the last four centuries" by R. Lanza, A. Meloni, and E. Tema. Phys. Earth Planet. Interiors 152, 116-120; Arrighi, S., 2004. The large sample archeomagnetic method applied to Neapolitan volcanoes and Aeolian Islands. PhD Thesis. University of Pisa, Italy, pp. 1-186). Age determination is based upon directional geomagnetic variation reconstructed from historically dated lavas in Southern Italy, and from archeological sites in Western Europe (Gallet, Y., Genevey, A., Le Goff, M., 2002. Three millennia of directional variation of the Earth's magnetic field in Western Europe as revealed by archeological artefacts. Phys. Earth Planet. Interiors 131, 81-89) relocated to Sicily. Results in the present paper were obtained on 12 sites including 185 samples weighing 0.5-1 kg, distributed over the Vulcanello platform lavas and pyroclastic cones, and on the lava flows from the Fossa cone. It is shown that the Vulcanello platform was built by nearly continuous activity between AD 1000 and 1250, which is more than a millennium younger than believed until now from questionable interpretation of imprecise historical accounts. Most of the lavas from the Fossa cone, whose ages were rather hypothetical or known with a large uncertainty, have erupted within the same period. However, the last "Pietre Cotte" obsidian flow is confirmed to date from 1720 ?? 30, in agreement with historical data (1739). ?? 2006.
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Eruptions of the last 2200 years at Vulcano and Vulcanello (Aeolian Islands, Italy) dated by high-accuracy archeomagnetism
Physics of the Earth and Planetary Interiors, 2006Co-Authors: Simone Arrighi, Jean-claude Tanguy, Mauro RosiAbstract:International audienceThe recent eruptive history of the Vulcano island (Southern Italy) was investigated through the high-accuracy “large sample” archeomagnetic method (Tanguy, J.C., Le Goff, M., Principe, C., Arrighi, S., Chillemi, V., Paiotti, A., La Delfa, S., Patanè, G., 2003. Archeomagnetic dating of Mediterranean volcanics of the last 2100 years: validity and limits. Earth Planet. Sci. Lett. 211, 111–124; Tanguy, J.C., Principe, C., Arrighi, S., 2005. Comment on “Historical measurements of the Earth's magnetic field compared with remanence directions from lava flows in Italy over the last four centuries” by R. Lanza, A. Meloni, and E. Tema. Phys. Earth Planet. Interiors 152, 116–120; Arrighi, S., 2004. The large sample archeomagnetic method applied to Neapolitan volcanoes and Aeolian Islands. PhD Thesis. University of Pisa, Italy, pp. 1–186). Age determination is based upon directional geomagnetic variation reconstructed from historically dated lavas in Southern Italy, and from archeological sites in Western Europe (Gallet, Y., Genevey, A., Le Goff, M., 2002. Three millennia of directional variation of the Earth's magnetic field in Western Europe as revealed by archeological artefacts. Phys. Earth Planet. Interiors 131, 81–89) relocated to Sicily. Results in the present paper were obtained on 12 sites including 185 samples weighing 0.5–1 kg, distributed over the Vulcanello platform lavas and pyroclastic cones, and on the lava flows from the Fossa cone. It is shown that the Vulcanello platform was built by nearly continuous activity between AD 1000 and 1250, which is more than a millennium younger than believed until now from questionable interpretation of imprecise historical accounts. Most of the lavas from the Fossa cone, whose ages were rather hypothetical or known with a large uncertainty, have erupted within the same period. However, the last “Pietre Cotte” obsidian flow is confirmed to date from 1720 ± 30, in agreement with historical data (1739)
Simone Arrighi - One of the best experts on this subject based on the ideXlab platform.
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Eruptions of the last 2200 years at Vulcano and Vulcanello (Aeolian Islands, Italy) dated by high-accuracy archeomagnetism
Physics of the Earth and Planetary Interiors, 2006Co-Authors: Simone Arrighi, Jean-claude Tanguy, Mauro RosiAbstract:The recent eruptive history of the Vulcano island (Southern Italy) was investigated through the high-accuracy “large sample” archeomagnetic method (Tanguy, J.C., Le Goff, M., Principe, C., Arrighi, S., Chillemi, V., Paiotti, A., La Delfa, S., Patane, G., 2003. Archeomagnetic dating of Mediterranean volcanics of the last 2100 years: validity and limits. Earth Planet. Sci. Lett. 211, 111–124; Tanguy, J.C., Principe, C., Arrighi, S., 2005. Comment on “Historical measurements of the Earth's magnetic field compared with remanence directions from lava flows in Italy over the last four centuries” by R. Lanza, A. Meloni, and E. Tema. Phys. Earth Planet. Interiors 152, 116–120; Arrighi, S., 2004. The large sample archeomagnetic method applied to Neapolitan volcanoes and Aeolian Islands. PhD Thesis. University of Pisa, Italy, pp. 1–186). Age determination is based upon directional geomagnetic variation reconstructed from historically dated lavas in Southern Italy, and from archeological sites in Western Europe (Gallet, Y., Genevey, A., Le Goff, M., 2002. Three millennia of directional variation of the Earth's magnetic field in Western Europe as revealed by archeological artefacts. Phys. Earth Planet. Interiors 131, 81–89) relocated to Sicily. Results in the present paper were obtained on 12 sites including 185 samples weighing 0.5–1 kg, distributed over the Vulcanello platform lavas and pyroclastic cones, and on the lava flows from the Fossa cone. It is shown that the Vulcanello platform was built by nearly continuous activity between AD 1000 and 1250, which is more than a millennium younger than believed until now from questionable interpretation of imprecise historical accounts. Most of the lavas from the Fossa cone, whose ages were rather hypothetical or known with a large uncertainty, have erupted within the same period. However, the last “Pietre Cotte” obsidian flow is confirmed to date from 1720 ± 30, in agreement with historical data (1739).
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Eruptions of the last 2200 years at Vulcano and Vulcanello (Aeolian Islands, Italy) dated by high-accuracy archeomagnetism
Physics of the Earth and Planetary Interiors, 2006Co-Authors: Simone Arrighi, J-Y Tanguy, Mauro RosiAbstract:The recent eruptive history of the Vulcano island (Southern Italy) was investigated through the high-accuracy "large sample" archeomagnetic method (Tanguy, J.C., Le Goff, M., Principe, C., Arrighi, S., Chillemi, V., Paiotti, A., La Delfa, S., Patan??, G., 2003. Archeomagnetic dating of Mediterranean volcanics of the last 2100 years: validity and limits. Earth Planet. Sci. Lett. 211, 111-124; Tanguy, J.C., Principe, C., Arrighi, S., 2005. Comment on "Historical measurements of the Earth's magnetic field compared with remanence directions from lava flows in Italy over the last four centuries" by R. Lanza, A. Meloni, and E. Tema. Phys. Earth Planet. Interiors 152, 116-120; Arrighi, S., 2004. The large sample archeomagnetic method applied to Neapolitan volcanoes and Aeolian Islands. PhD Thesis. University of Pisa, Italy, pp. 1-186). Age determination is based upon directional geomagnetic variation reconstructed from historically dated lavas in Southern Italy, and from archeological sites in Western Europe (Gallet, Y., Genevey, A., Le Goff, M., 2002. Three millennia of directional variation of the Earth's magnetic field in Western Europe as revealed by archeological artefacts. Phys. Earth Planet. Interiors 131, 81-89) relocated to Sicily. Results in the present paper were obtained on 12 sites including 185 samples weighing 0.5-1 kg, distributed over the Vulcanello platform lavas and pyroclastic cones, and on the lava flows from the Fossa cone. It is shown that the Vulcanello platform was built by nearly continuous activity between AD 1000 and 1250, which is more than a millennium younger than believed until now from questionable interpretation of imprecise historical accounts. Most of the lavas from the Fossa cone, whose ages were rather hypothetical or known with a large uncertainty, have erupted within the same period. However, the last "Pietre Cotte" obsidian flow is confirmed to date from 1720 ?? 30, in agreement with historical data (1739). ?? 2006.
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Eruptions of the last 2200 years at Vulcano and Vulcanello (Aeolian Islands, Italy) dated by high-accuracy archeomagnetism
Physics of the Earth and Planetary Interiors, 2006Co-Authors: Simone Arrighi, Jean-claude Tanguy, Mauro RosiAbstract:International audienceThe recent eruptive history of the Vulcano island (Southern Italy) was investigated through the high-accuracy “large sample” archeomagnetic method (Tanguy, J.C., Le Goff, M., Principe, C., Arrighi, S., Chillemi, V., Paiotti, A., La Delfa, S., Patanè, G., 2003. Archeomagnetic dating of Mediterranean volcanics of the last 2100 years: validity and limits. Earth Planet. Sci. Lett. 211, 111–124; Tanguy, J.C., Principe, C., Arrighi, S., 2005. Comment on “Historical measurements of the Earth's magnetic field compared with remanence directions from lava flows in Italy over the last four centuries” by R. Lanza, A. Meloni, and E. Tema. Phys. Earth Planet. Interiors 152, 116–120; Arrighi, S., 2004. The large sample archeomagnetic method applied to Neapolitan volcanoes and Aeolian Islands. PhD Thesis. University of Pisa, Italy, pp. 1–186). Age determination is based upon directional geomagnetic variation reconstructed from historically dated lavas in Southern Italy, and from archeological sites in Western Europe (Gallet, Y., Genevey, A., Le Goff, M., 2002. Three millennia of directional variation of the Earth's magnetic field in Western Europe as revealed by archeological artefacts. Phys. Earth Planet. Interiors 131, 81–89) relocated to Sicily. Results in the present paper were obtained on 12 sites including 185 samples weighing 0.5–1 kg, distributed over the Vulcanello platform lavas and pyroclastic cones, and on the lava flows from the Fossa cone. It is shown that the Vulcanello platform was built by nearly continuous activity between AD 1000 and 1250, which is more than a millennium younger than believed until now from questionable interpretation of imprecise historical accounts. Most of the lavas from the Fossa cone, whose ages were rather hypothetical or known with a large uncertainty, have erupted within the same period. However, the last “Pietre Cotte” obsidian flow is confirmed to date from 1720 ± 30, in agreement with historical data (1739)
Nuno C. Santos - One of the best experts on this subject based on the ideXlab platform.
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The HARPS search for southern extra-solar Planets XXII. Multiple Planet systems from the HARPS volume limited sample
Astronomy and Astrophysics, 2010Co-Authors: G. Lo Curto, Michel Mayor, Willy Benz, F. Bouchy, Christophe Lovis, C. Moutou, Dominique Naef, Francesco Pepe, D. Queloz, Nuno C. SantosAbstract:We present the detections of three multiple systems within the HARPS volume-limited sample. Among the six Planets discussed in this paper, we have identified a “super-Earth” Planet with a minimum mass of 6.6 M(Earth) and a “Neptune” Planet with minimum mass of 18 M(Earth), both orbiting their parent stars within a distance of 0.05 AU and a period of approximately four days. These detections strengthen the argument that low-mass Planets are primarily found in multiple-Planetary systems.
Christian Hensen - One of the best experts on this subject based on the ideXlab platform.
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corrigendum to impact of hot fluid advection on hydrocarbon gas production and seepage in mud volcano sediments of thick cenozoic deltas Earth Planet sci lett 341 344 2012 139 157
Earth and Planetary Science Letters, 2012Co-Authors: Marianne Nuzzo, Marcus Elvert, Mark Schmidt, Florian Scholz, Anja Reitz, Kaiuwe Hinrichs, Christian HensenAbstract:Corrigendum to ‘‘Impact of hot fluid advection on hydrocarbon gas production and seepage in mud volcano sediments of thick Cenozoic deltas’’ [Earth Planet. Sci. Lett. 341–344 (2012) 139–157] Marianne Nuzzo , Marcus Elvert , Mark Schmidt , Florian Scholz , Anja Reitz , Kai-Uwe Hinrichs , Christian Hensen a a GEOMAR Helmholtz Centre for Ocean Research Kiel, Wischhofstrabe 1-3, D-24148 Kiel, Germany b Organic Geochemistry Group, Department of Geosciences and MARUM—Centre for Marine Environmental Sciences, University of Bremen, Leobener Str., D-28359 Bremen, Germany
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Corrigendum to “Impact of hot fluid advection on hydrocarbon gas production and seepage in mud volcano sediments of thick Cenozoic deltas” [Earth Planet. Sci. Lett. 341–344 (2012) 139–157]
Earth and Planetary Science Letters, 2012Co-Authors: Marianne Nuzzo, Marcus Elvert, Mark Schmidt, Florian Scholz, Anja Reitz, Kaiuwe Hinrichs, Christian HensenAbstract:Corrigendum to ‘‘Impact of hot fluid advection on hydrocarbon gas production and seepage in mud volcano sediments of thick Cenozoic deltas’’ [Earth Planet. Sci. Lett. 341–344 (2012) 139–157] Marianne Nuzzo , Marcus Elvert , Mark Schmidt , Florian Scholz , Anja Reitz , Kai-Uwe Hinrichs , Christian Hensen a a GEOMAR Helmholtz Centre for Ocean Research Kiel, Wischhofstrabe 1-3, D-24148 Kiel, Germany b Organic Geochemistry Group, Department of Geosciences and MARUM—Centre for Marine Environmental Sciences, University of Bremen, Leobener Str., D-28359 Bremen, Germany
G. Lo Curto - One of the best experts on this subject based on the ideXlab platform.
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The HARPS search for southern extra-solar Planets XXII. Multiple Planet systems from the HARPS volume limited sample
Astronomy and Astrophysics, 2010Co-Authors: G. Lo Curto, Michel Mayor, Willy Benz, F. Bouchy, Christophe Lovis, C. Moutou, Dominique Naef, Francesco Pepe, D. Queloz, Nuno C. SantosAbstract:We present the detections of three multiple systems within the HARPS volume-limited sample. Among the six Planets discussed in this paper, we have identified a “super-Earth” Planet with a minimum mass of 6.6 M(Earth) and a “Neptune” Planet with minimum mass of 18 M(Earth), both orbiting their parent stars within a distance of 0.05 AU and a period of approximately four days. These detections strengthen the argument that low-mass Planets are primarily found in multiple-Planetary systems.
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XXII. Multiple Planet systems from the HARPS volume limited sample
2010Co-Authors: G. Lo Curto, Michel Mayor, F. Bouchy, C. Moutou, Dominique Naef, Francesco Pepe, D. Segransan, Stéphane UdryAbstract:We present the detections of three multiple systems within the HARPS volume-limited sample. Among the six Planets discussed in this paper, we have identified a “super-Earth” Planet with a minimum mass of 6.6 MEarth and a “Neptune” Planet with minimum mass of 18 MEarth, both orbiting their parent stars within a distance of 0.05 AU and a period of approximately four days. These detections strengthen the argument that low-mass Planets are primarily found in multiple-Planetary systems.
