What is he best known for?
The fields of study he is best known for:
- Basalt
- Igneous rock
- Sedimentary rock
His primary areas of investigation include Geochemistry, Crust, Mantle, Zircon and Early Earth.
His Geochemistry research integrates issues from Chondrite and Meteorite.
His research investigates the connection between Crust and topics such as Archean that intersect with problems in Protolith, Gneiss and Incompatible element.
His study in Mantle is interdisciplinary in nature, drawing from both Passive margin, Isotope fractionation and Mafic.
His Zircon research incorporates themes from Subduction, Earth science and Proterozoic.
Jeffrey D. Vervoort has researched Proterozoic in several fields, including Laurentia and Craton.
His most cited work include:
- The 176Lu decay constant determined by Lu–Hf and U–Pb isotope systematics of Precambrian mafic intrusions (1735 citations)
- The Lu–Hf and Sm–Nd isotopic composition of CHUR: Constraints from unequilibrated chondrites and implications for the bulk composition of terrestrial planets (1720 citations)
- Evolution of the depleted mantle: Hf isotope evidence from juvenile rocks through time (1013 citations)
What are the main themes of his work throughout his whole career to date?
Jeffrey D. Vervoort mainly investigates Geochemistry, Zircon, Geochronology, Paleontology and Crust.
His Geochemistry study integrates concerns from other disciplines, such as Subduction and Petrology.
His Zircon study combines topics from a wide range of disciplines, such as Archean, Craton, Magmatism, Gneiss and Terrane.
His research in Geochronology intersects with topics in Metamorphic facies and Monazite.
The Crust study combines topics in areas such as Proterozoic and Early Earth.
Volcano and Radiogenic nuclide is closely connected to Basalt in his research, which is encompassed under the umbrella topic of Mantle.
He most often published in these fields:
- Geochemistry (71.37%)
- Zircon (34.36%)
- Geochronology (20.26%)
What were the highlights of his more recent work (between 2016-2021)?
- Geochemistry (71.37%)
- Zircon (34.36%)
- Paleontology (16.30%)
In recent papers he was focusing on the following fields of study:
Jeffrey D. Vervoort mostly deals with Geochemistry, Zircon, Paleontology, Geochronology and Crust.
His study in Metamorphism, Metamorphic rock, Monazite, Mantle and Early Earth is carried out as part of his Geochemistry studies.
His work carried out in the field of Early Earth brings together such families of science as Acasta Gneiss and Hadean.
The study incorporates disciplines such as Sedimentary rock, Craton, Shear zone, Magmatism and Terrane in addition to Zircon.
Jeffrey D. Vervoort studies Crust, namely Continental crust.
His work deals with themes such as Basalt and Mafic, which intersect with Continental crust.
Between 2016 and 2021, his most popular works were:
- Using the magmatic record to constrain the growth of continental crust—The Eoarchean zircon Hf record of Greenland (49 citations)
- Coupled zircon Lu–Hf and U–Pb isotopic analyses of the oldest terrestrial crust, the >4.03 Ga Acasta Gneiss Complex (42 citations)
- Proterozoic crustal evolution of central East Antarctica: Age and isotopic evidence from glacial igneous clasts, and links with Australia and Laurentia (25 citations)
In his most recent research, the most cited papers focused on:
- Basalt
- Igneous rock
- Sedimentary rock
His primary scientific interests are in Geochemistry, Zircon, Mantle, Geochronology and Continental crust.
His Geochemistry research is multidisciplinary, incorporating perspectives in Subduction and Eclogite.
Jeffrey D. Vervoort interconnects Radiogenic nuclide, Sedimentary rock, Cretaceous, Early Earth and Shear zone in the investigation of issues within Zircon.
His research integrates issues of Basalt and Amphibole in his study of Mantle.
His Geochronology research is multidisciplinary, relying on both Provenance, Sedimentation, Spinel, Sedimentary depositional environment and Volcanic arc.
His work in Continental crust addresses issues such as Mafic, which are connected to fields such as Silicic, Magma and Granulite.
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