What is he best known for?
The fields of study he is best known for:
- Basalt
- Igneous rock
- Volcano
The scientist’s investigation covers issues in Geochemistry, Mineralogy, Peridotite, Mantle and Basalt.
He works on Geochemistry which deals in particular with Metasomatism.
His Mineralogy study which covers Analytical chemistry that intersects with Diopside.
His Peridotite research integrates issues from Melt migration and Incompatible element.
His studies deal with areas such as Adakite and Igneous rock as well as Mantle.
His Basalt research focuses on Trace element and how it connects with Lava.
His most cited work include:
- Reaction between slab-derived melts and peridotite in the mantle wedge: experimental constraints at 3.8 GPa (1209 citations)
- Melting in the oceanic upper mantle: An ion microprobe study of diopsides in abyssal peridotites (1019 citations)
- 143Nd/146Nd, a natural tracer: an application to oceanic basalts* (779 citations)
What are the main themes of his work throughout his whole career to date?
His primary areas of study are Geochemistry, Mineralogy, Mantle, Basalt and Peridotite.
His Geochemistry study frequently draws connections to other fields, such as Oceanic crust.
Nobumichi Shimizu interconnects Crystallization, Silicate and Analytical chemistry in the investigation of issues within Mineralogy.
His work in Mantle covers topics such as Lithosphere which are related to areas like Seamount.
He studied Basalt and Igneous rock that intersect with Volcanic rock.
His work deals with themes such as Abyssal zone, Adakite, Spinel and Incompatible element, which intersect with Peridotite.
He most often published in these fields:
- Geochemistry (53.70%)
- Mineralogy (40.12%)
- Mantle (35.19%)
What were the highlights of his more recent work (between 2010-2021)?
- Mineralogy (40.12%)
- Mantle (35.19%)
- Geochemistry (53.70%)
In recent papers he was focusing on the following fields of study:
Nobumichi Shimizu mainly investigates Mineralogy, Mantle, Geochemistry, Basalt and Melt inclusions.
Nobumichi Shimizu studies Mineralogy, focusing on Olivine in particular.
Nobumichi Shimizu usually deals with Mantle and limits it to topics linked to Earth science and Astrobiology.
Nobumichi Shimizu has included themes like Hotspot and Oceanic crust in his Geochemistry study.
The concepts of his Basalt study are interwoven with issues in Fracture zone, Transition zone, Isotope analysis, Isotopic signature and Abyssal zone.
His study in Melt inclusions is interdisciplinary in nature, drawing from both Submarine eruption, Mafic and Amphibole.
Between 2010 and 2021, his most popular works were:
- Rapid reequilibration of H2O and oxygen fugacity in olivine-hosted melt inclusions (210 citations)
- Evidence for Microbial Carbon and Sulfur Cycling in Deeply Buried Ridge Flank Basalt (143 citations)
- Post-entrapment modification of volatiles and oxygen fugacity in olivine-hosted melt inclusions (141 citations)
In his most recent research, the most cited papers focused on:
- Basalt
- Igneous rock
- Volcano
His primary scientific interests are in Mantle, Mineralogy, Basalt, Silicate and Geochemistry.
His primary area of study in Mantle is in the field of Melt inclusions.
His Mineralogy research is multidisciplinary, relying on both Mineral redox buffer and Analytical chemistry.
His research in Basalt focuses on subjects like Trace element, which are connected to Subduction.
His Geochemistry study frequently intersects with other fields, such as Oceanic crust.
His Olivine study combines topics from a wide range of disciplines, such as Partition coefficient and Lile.
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