What is he best known for?
The fields of study he is best known for:
- Basalt
- Igneous rock
- Volcano
His main research concerns Geochemistry, Mantle, Continental crust, Oceanic crust and Crustal recycling.
His study in Metasomatism, Peridotite and Olivine is carried out as part of his Geochemistry studies.
Andreas Stracke is interested in Partial melting, which is a field of Mantle.
His work in Continental crust addresses subjects such as Basalt, which are connected to disciplines such as Trace element.
His Oceanic crust research is multidisciplinary, incorporating elements of Earth's internal heat budget, Isotope geochemistry, Hotspot and Crust.
His Crustal recycling research includes elements of Planetary differentiation, Mantle convection, Mantle wedge and Transition zone.
His most cited work include:
- Composition of the depleted mantle (1150 citations)
- Composition of the depleted mantle (1150 citations)
- Determination of Reference Values for NIST SRM 610–617 Glasses Following ISO Guidelines (930 citations)
What are the main themes of his work throughout his whole career to date?
Andreas Stracke mainly investigates Geochemistry, Mantle, Basalt, Continental crust and Trace element.
Geochemistry is frequently linked to Oceanic crust in his study.
His Mantle study incorporates themes from Asthenosphere, Petrology and Crust.
His Crust research focuses on subjects like Adakite, which are linked to Isotope geochemistry.
His work carried out in the field of Basalt brings together such families of science as Mineralogy, Amphibole and Upwelling.
His work deals with themes such as Oceanic plateau and Archean, which intersect with Continental crust.
He most often published in these fields:
- Geochemistry (87.61%)
- Mantle (66.37%)
- Basalt (50.44%)
What were the highlights of his more recent work (between 2018-2021)?
- Geochemistry (87.61%)
- Mantle (66.37%)
- Basalt (50.44%)
In recent papers he was focusing on the following fields of study:
Andreas Stracke mainly focuses on Geochemistry, Mantle, Basalt, Crust and Continental crust.
Andreas Stracke studies Geochemistry, focusing on Carbonatite in particular.
The concepts of his Mantle study are interwoven with issues in Archean and Oceanic crust.
His Basalt research integrates issues from Trace element and Radiogenic nuclide.
As part of the same scientific family, Andreas Stracke usually focuses on Trace element, concentrating on Lava and intersecting with Olivine.
His studies in Continental crust integrate themes in fields like Metasomatism and Oceanic plateau.
Between 2018 and 2021, his most popular works were:
- Ubiquitous ultra-depleted domains in Earth’s mantle (18 citations)
- Lack of late-accreted material as the origin of 182W excesses in the Archean mantle: Evidence from the Pilbara Craton, Western Australia (9 citations)
- K-rich hydrous mantle lithosphere beneath the Ontong Java Plateau: Significance for the genesis of oceanic basalts and Archean continents (8 citations)
In his most recent research, the most cited papers focused on:
- Basalt
- Igneous rock
- Plate tectonics
His primary areas of investigation include Geochemistry, Mantle, Basalt, Plate tectonics and Kimberlite.
The study of Geochemistry is intertwined with the study of Mantle plume in a number of ways.
The various areas that Andreas Stracke examines in his Mantle plume study include Melt inclusions and Partial melting, Incompatible element.
His research integrates issues of Crust and Oceanic crust in his study of Mantle.
His Metasomatism study integrates concerns from other disciplines, such as Oceanic plateau and Continental crust.
His Archean research is multidisciplinary, relying on both Magma ocean and Radiogenic nuclide.
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