What is he best known for?
The fields of study he is best known for:
- Basalt
- Volcano
- Igneous rock
Fabrizio Innocenti spends much of his time researching Geochemistry, Volcanic rock, Volcanism, Subduction and Earth science.
His Geochemistry research includes themes of Geomorphology and Asthenosphere.
His Volcanism study also includes fields such as
- Volcano together with Petrology,
- Quaternary which intersects with area such as Plateau, Outcrop, Period and Rift.
As part of the same scientific family, Fabrizio Innocenti usually focuses on Subduction, concentrating on Magmatism and intersecting with Laccolith and Incompatible element.
His studies in Earth science integrate themes in fields like Flood basalt, Volcanic hazards and Isotopes of strontium.
His biological study spans a wide range of topics, including Trace element and Lithosphere.
His most cited work include:
- Geochemical and petrological evidence of the subduction of delaminated Adriatic continental lithosphere in the genesis of the Neogene-Quaternary magmatism of central Italy (372 citations)
- Tertiary to Quaternary evolution of volcanism in the Aegean region (365 citations)
- Evolution of Eolian arc volcanism (Southern Tyrrhenian Sea) (253 citations)
What are the main themes of his work throughout his whole career to date?
Fabrizio Innocenti mainly investigates Geochemistry, Volcanic rock, Petrology, Volcano and Mantle.
His Geochemistry study incorporates themes from Magmatism, Subduction and Earth science.
His Volcanic rock research focuses on subjects like Quaternary, which are linked to Geomorphology.
Fabrizio Innocenti interconnects Petrogenesis, Geophysics, Magma chamber, Magma and Terrane in the investigation of issues within Petrology.
In Volcano, Fabrizio Innocenti works on issues like Volcanism, which are connected to Neogene.
His research investigates the connection with Mantle and areas like Mantle wedge which intersect with concerns in Volcanic arc.
He most often published in these fields:
- Geochemistry (59.59%)
- Volcanic rock (24.66%)
- Petrology (19.86%)
What were the highlights of his more recent work (between 2004-2015)?
- Geochemistry (59.59%)
- Subduction (15.75%)
- Mantle (16.44%)
In recent papers he was focusing on the following fields of study:
His scientific interests lie mostly in Geochemistry, Subduction, Mantle, Mantle wedge and Lithosphere.
His Geochemistry research is multidisciplinary, relying on both Earth science, Petrology and Late Miocene.
His Subduction research is multidisciplinary, incorporating perspectives in Pleistocene, Intraplate earthquake, Rift and Magmatism.
His Mantle study integrates concerns from other disciplines, such as Crust and Asthenosphere.
The various areas that Fabrizio Innocenti examines in his Mantle wedge study include Incompatible element, Volcanic arc, Geophysics and Slab window.
His Lithosphere study deals with Geodynamics intersecting with African Plate.
Between 2004 and 2015, his most popular works were:
- Evolution of the Main Ethiopian Rift in the frame of Afar and Kenya rifts propagation (161 citations)
- Neogene and Quaternary volcanism in Western Anatolia: Magma sources and geodynamic evolution (134 citations)
- Carbonatites in a subduction system: The Pleistocene alvikites from Mt. Vulture (southern Italy) (80 citations)
In his most recent research, the most cited papers focused on:
- Basalt
- Igneous rock
- Volcano
His primary areas of study are Geochemistry, Mantle, Subduction, Lithosphere and Seismology.
The Geochemistry study combines topics in areas such as Intraplate earthquake and Mantle wedge.
His Subduction study frequently draws connections between adjacent fields such as Magmatism.
Fabrizio Innocenti works mostly in the field of Lithosphere, limiting it down to concerns involving Geodynamics and, occasionally, Asthenosphere, African Plate and Extensional tectonics.
His Seismology research focuses on Petrology and how it connects with Tectonics, Sinistral and dextral, Structural geology and Geothermal gradient.
The study incorporates disciplines such as Pyroclastic rock, Carbonatite, Igneous rock and Slab window in addition to Volcanic rock.
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