Roberto Isaia mostly deals with Volcano, Caldera, Tephra, Seismology and Volcanic rock. The various areas that Roberto Isaia examines in his Caldera study include Hypocenter, Epicenter and Vertical displacement. His Tephra study necessitates a more in-depth grasp of Paleontology.
His study on Volcanism, Explosive eruption, Induced seismicity and Focal mechanism is often connected to Simple shear as part of broader study in Seismology. He combines subjects such as Block, Volcanic hazards, Effusive eruption, Fault and Series with his study of Explosive eruption. His work is dedicated to discovering how Volcanic rock, Pyroclastic rock are connected with Magma and Igneous rock and other disciplines.
Roberto Isaia spends much of his time researching Caldera, Volcano, Seismology, Geochemistry and Pyroclastic rock. His Caldera research integrates issues from Volcanic rock, Volcanic hazards, Volcanism, Petrology and Geomorphology. Paleontology covers Roberto Isaia research in Volcano.
In the subject of general Seismology, his work in Fumarole is often linked to Probabilistic logic, Event, Uncertainty quantification and Electrical resistivity tomography, thereby combining diverse domains of study. His work in the fields of Geochemistry, such as Phreatomagmatic eruption, Volcanology and Apatite, overlaps with other areas such as Biological dispersal. In general Pyroclastic rock study, his work on Eruption column often relates to the realm of Term, thereby connecting several areas of interest.
His primary areas of investigation include Caldera, Volcano, Seismology, Geochemistry and Magma. His research integrates issues of Trachyte and Deformation in his study of Caldera. Volcano is the subject of his research, which falls under Paleontology.
His work on Fumarole, Eruption column and Volcanic hazards as part of general Seismology study is frequently linked to Electrical resistivity tomography and Duration, bridging the gap between disciplines. His Pyroclastic rock and Volcanic explosivity index study, which is part of a larger body of work in Geochemistry, is frequently linked to Gravimetric analysis, bridging the gap between disciplines. Roberto Isaia has researched Magma in several fields, including Clastic rock, Volcanism, Petrology, Pumice and Tephra.
His primary areas of study are Caldera, Volcano, Magma, Deformation and Geochemistry. His Caldera research incorporates elements of Fumarole, Sea level, Petrology, Water content and Subsidence. His Volcano study is concerned with the larger field of Seismology.
His Magma research includes themes of Pyroclastic rock, Clastic rock, Trachyte, Melt inclusions and Pumice. His Deformation study incorporates themes from Vertical displacement, Sediment, Volcano tectonics and Tectonics. His study in Volcanic ash, Tephra, Dense-rock equivalent and Volcanic explosivity index falls under the purview of Geochemistry.
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Volcanism and deformation since 12,000 years at the Campi Flegrei caldera (Italy)
M.A Di Vito;R Isaia;G Orsi;J Southon.
Journal of Volcanology and Geothermal Research (1999)
Volcanic hazard assessment at the restless Campi Flegrei caldera
Giovanni Orsi;Mauro Antonio Di Vito;Roberto Isaia.
Bulletin of Volcanology (2004)
The Agnano-Monte Spina eruption (4100 years BP) in the restless Campi Flegrei caldera (Italy)
S de Vita;G Orsi;L Civetta;A Carandente.
Journal of Volcanology and Geothermal Research (1999)
Chemical and Sr-isotopical evolution of the Phlegraean magmatic system before the Campanian Ignimbrite and the Neapolitan Yellow Tuff eruptions
L Pappalardo;L Civetta;M D'Antonio;A Deino.
Journal of Volcanology and Geothermal Research (1999)
Tephrostratigraphy and glass compositions of post-15 kyr Campi Flegrei eruptions: implications for eruption history and chronostratigraphic markers
V. C. Smith;R. Isaia;N. J. G. Pearce.
Quaternary Science Reviews (2011)
Short-term ground deformations and seismicity in the resurgent Campi Flegrei caldera (Italy): an example of active block-resurgence in a densely populated area
G. Orsi;L. Civetta;C. Del Gaudio;S. de Vita.
Journal of Volcanology and Geothermal Research (1999)
The Campanian Ignimbrite and Codola tephra layers: Two temporal/stratigraphic markers for the Early Upper Palaeolithic in southern Italy and eastern Europe
Biagio Giaccio;Roberto Isaia;Francesco G. Fedele;Emanuele Di Canzio.
Journal of Volcanology and Geothermal Research (2008)
The present state of the magmatic system of the Campi Flegrei caldera based on a reconstruction of its behavior in the past 12 ka
M D'Antonio;L Civetta;G Orsi;L Pappalardo.
Journal of Volcanology and Geothermal Research (1999)
High-precision 14 C and 40 Ar/ 39 Ar dating of the Campanian Ignimbrite (Y-5) reconciles the time-scales of climatic-cultural processes at 40 ka
Biagio Giaccio;Irka Hajdas;Roberto Isaia;Alan Deino.
Scientific Reports (2017)
Caldera unrest prior to intense volcanism in Campi Flegrei (Italy) at 4.0 ka B.P.: Implications for caldera dynamics and future eruptive scenarios
Roberto Isaia;Paola Marianelli;Alessandro Sbrana.
Geophysical Research Letters (2009)
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