What is he best known for?
The fields of study he is best known for:
- Basalt
- Volcano
- Igneous rock
His primary areas of investigation include Geochemistry, Caldera, Volcano, Volcanic rock and Pyroclastic rock.
Massimo D'Antonio works mostly in the field of Geochemistry, limiting it down to topics relating to Subduction and, in certain cases, Seamount, as a part of the same area of interest.
Massimo D'Antonio has included themes like Trachyte and Phreatomagmatic eruption in his Caldera study.
Latite and Explosive eruption are the subjects of his Volcano studies.
His studies in Volcanic rock integrate themes in fields like Geochronology, Igneous differentiation and Incompatible element.
His study in Pyroclastic rock is interdisciplinary in nature, drawing from both Magma and Igneous rock.
His most cited work include:
- Volcanism and deformation since 12,000 years at the Campi Flegrei caldera (Italy) (348 citations)
- Source contamination and mantle heterogeneity in the genesis of Italian potassic and ultrapotassic volcanic rocks: Sr–Nd–Pb isotope data from Roman Province and Southern Tuscany (184 citations)
- Chemical and Sr-isotopical evolution of the Phlegraean magmatic system before the Campanian Ignimbrite and the Neapolitan Yellow Tuff eruptions (183 citations)
What are the main themes of his work throughout his whole career to date?
Geochemistry, Caldera, Volcano, Mantle and Magma are his primary areas of study.
In his study, Ophiolite is strongly linked to Subduction, which falls under the umbrella field of Geochemistry.
His Caldera study combines topics from a wide range of disciplines, such as Fractional crystallization, Pyroclastic rock, Phreatomagmatic eruption and Trachyte.
As a part of the same scientific study, Massimo D'Antonio usually deals with the Volcano, concentrating on Volcanism and frequently concerns with Block.
His Mantle research includes themes of Slab, Isotope geochemistry and Magmatism.
His Magma research incorporates elements of Petrology and Igneous differentiation.
He most often published in these fields:
- Geochemistry (92.98%)
- Caldera (38.60%)
- Volcano (34.21%)
What were the highlights of his more recent work (between 2017-2021)?
- Geochemistry (92.98%)
- Volcano (34.21%)
- Mafic (22.81%)
In recent papers he was focusing on the following fields of study:
Massimo D'Antonio mainly investigates Geochemistry, Volcano, Mafic, Isotope geochemistry and Crust.
His work in the fields of Geochemistry, such as Mantle, Olivine and Basalt, intersects with other areas such as Isotope analysis.
His research in the fields of Magma and Volcanic rock overlaps with other disciplines such as Human migration.
His work in Isotope geochemistry addresses subjects such as Hydrothermal circulation, which are connected to disciplines such as Back-arc basin, Facies and Incompatible element.
His Crust research is multidisciplinary, relying on both Pyroclastic rock, Petrology and Zircon.
Massimo D'Antonio focuses mostly in the field of Petrology, narrowing it down to topics relating to Volatiles and, in certain cases, Caldera and Trachyte.
Between 2017 and 2021, his most popular works were:
- Gravity modeling finds a large magma body in the deep crust below the Gulf of Naples, Italy (16 citations)
- Sr-Nd isotopic fingerprinting as a tool for ceramic provenance: Its application on raw materials, ceramic replicas and ancient pottery (14 citations)
- Sr-Nd isotopic fingerprinting as a tool for ceramic provenance: Its application on raw materials, ceramic replicas and ancient pottery (14 citations)
In his most recent research, the most cited papers focused on:
- Basalt
- Volcano
- Igneous rock
Massimo D'Antonio spends much of his time researching Geochemistry, Pottery, Isotope analysis, Provenance and Radiogenic Isotopes.
His study in the field of Igneous differentiation, Trace element, Magma and Volcano is also linked to topics like High resolution.
His primary area of study in Pottery is in the field of Archaeological pottery.
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