What is he best known for?
The fields of study he is best known for:
- Igneous rock
- Basalt
- Magma
Riccardo Vannucci mainly investigates Geochemistry, Mineralogy, Mantle, Analytical chemistry and Pargasite.
His Geochemistry research focuses on Oceanic crust and how it connects with Flux melting and Continental crust.
His work on Electron microprobe as part of general Mineralogy research is frequently linked to Partition coefficient, bridging the gap between disciplines.
His study in Mantle is interdisciplinary in nature, drawing from both Petrology, Olivine and Ultramafic rock.
Riccardo Vannucci has researched Analytical chemistry in several fields, including Boron, Beryllium, Ionization and Partial melting.
His Pargasite research focuses on Kaersutite and how it relates to Cummingtonite.
His most cited work include:
- MPI-DING reference glasses for in situ microanalysis: New reference values for element concentrations and isotope ratios (743 citations)
- Growth of early continental crust controlled by melting of amphibolite in subduction zones (665 citations)
- The Finero phlogopite-peridotite massif: an example of subduction-related metasomatism (226 citations)
What are the main themes of his work throughout his whole career to date?
Riccardo Vannucci mostly deals with Geochemistry, Mantle, Peridotite, Metasomatism and Trace element.
His studies deal with areas such as Asthenosphere, Igneous rock and Crust as well as Mantle.
He works mostly in the field of Peridotite, limiting it down to topics relating to Pargasite and, in certain cases, Kaersutite, as a part of the same area of interest.
Riccardo Vannucci has included themes like Lile, Phlogopite, Mantle wedge and Mantle plume in his Metasomatism study.
The Trace element study combines topics in areas such as Fractional crystallization and Mineralogy, Petrography.
While the research belongs to areas of Mineralogy, Riccardo Vannucci spends his time largely on the problem of Analytical chemistry, intersecting his research to questions surrounding Ionization.
He most often published in these fields:
- Geochemistry (75.17%)
- Mantle (45.64%)
- Peridotite (29.53%)
What were the highlights of his more recent work (between 2009-2019)?
- Geochemistry (75.17%)
- Mantle (45.64%)
- Peridotite (29.53%)
In recent papers he was focusing on the following fields of study:
Geochemistry, Mantle, Peridotite, Trace element and Metasomatism are his primary areas of study.
In his works, he undertakes multidisciplinary study on Geochemistry and Sapphirine.
His work carried out in the field of Mantle brings together such families of science as Eclogite, Olivine and Crust.
Riccardo Vannucci interconnects Pargasite, Massif, Igneous rock and Petrology in the investigation of issues within Peridotite.
His Trace element research is multidisciplinary, incorporating elements of Lile and Incompatible element.
His study in Partial melting extends to Metasomatism with its themes.
Between 2009 and 2019, his most popular works were:
- Crystal recycling in the steady-state system of the active Stromboli volcano: a 2.5-ka story inferred from in situ Sr-isotope and trace element data (38 citations)
- Age and geochemistry of mantle peridotites and diorite dykes from the Baldissero body: Insights into the Paleozoic–Mesozoic evolution of the Southern Alps (36 citations)
- Trace-element partitioning between plagioclase, alkali feldspar, Ti-magnetite, biotite, apatite, and evolved potassic liquids from Campi Flegrei (Southern Italy) (27 citations)
In his most recent research, the most cited papers focused on:
- Igneous rock
- Basalt
- Volcano
Riccardo Vannucci mainly investigates Geochemistry, Trace element, Mantle, Peridotite and Metasomatism.
He performs integrative study on Geochemistry and Porphyritic.
The concepts of his Trace element study are interwoven with issues in Lile and Incompatible element.
His studies in Peridotite integrate themes in fields like Pargasite, Massif and Igneous rock.
His Pargasite research is multidisciplinary, incorporating perspectives in Diorite, Mafic and Partial melting.
His research investigates the link between Metasomatism and topics such as Olivine that cross with problems in Xenolith, Eclogite and Mantle wedge.
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