Geochemistry, Zircon, Archean, Gneiss and Sensitive high-resolution ion microprobe are his primary areas of study. As part of his studies on Geochemistry, Hiroshi Hidaka often connects relevant areas like Mineralogy. In his research, Oklo, Lanthanide and Sediment is intimately related to Uranium, which falls under the overarching field of Mineralogy.
The Zircon study combines topics in areas such as Migmatite, Craton and Terrane. His Craton study integrates concerns from other disciplines, such as Orogeny and Protolith. His Sensitive high-resolution ion microprobe study combines topics from a wide range of disciplines, such as Radiometric dating and Geochronology.
His primary areas of study are Geochemistry, Zircon, Oklo, Mineralogy and Meteorite. His Geochemistry research is multidisciplinary, relying on both Sensitive high-resolution ion microprobe and Uraninite. His research integrates issues of Metamorphic rock, Archean, Craton and Geochronology in his study of Zircon.
The various areas that Hiroshi Hidaka examines in his Oklo study include Radiochemistry, Uranium, Isotope and Natural. His Mineralogy study frequently draws connections to adjacent fields such as Radiogenic nuclide. His Meteorite study incorporates themes from Neutron capture and Neutron.
The scientist’s investigation covers issues in Geochemistry, Zircon, Meteorite, Metamorphism and Astrobiology. His work deals with themes such as Barium, Craton and Basement, which intersect with Geochemistry. His studies in Zircon integrate themes in fields like Metamorphic rock, Gneiss and Archean.
His Meteorite research is multidisciplinary, incorporating perspectives in Neutron, Aqueous solution and Meteoroid. His Parent body research is multidisciplinary, incorporating elements of Abundance of the chemical elements, Mineralogy and Partial melting. His research in Chondrite intersects with topics in Radiochemistry and Natural abundance.
Hiroshi Hidaka mainly investigates Zircon, Geochemistry, Metamorphism, Metamorphic rock and Mineralogy. His study in Zircon is interdisciplinary in nature, drawing from both Mesosiderite, Ordovician and Silicate. His Geochemistry study focuses on Monazite in particular.
His work is dedicated to discovering how Metamorphism, Crust are connected with Migmatite, Earth science, Isochron dating and Dharwar Craton and other disciplines. His work investigates the relationship between Mineralogy and topics such as Parent body that intersect with problems in Radiochemistry, Barium, Extinct radionuclide and Chondrule. His Craton study combines topics in areas such as Proterozoic and Archean.
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Atomic weights of the elements. Review 2000 (IUPAC Technical Report)
John R. de Laeter;John Karl Böhlke;P. De Bièvre;H. Hidaka.
Pure and Applied Chemistry (2009)
Estrogen increases endothelial nitric oxide by a receptor-mediated system.
T Hayashi;K Yamada;T Esaki;M Kuzuya.
Biochemical and Biophysical Research Communications (1995)
Isotopic Compositions of the Elements, 2001
J. K. Böhlke;J. R. de Laeter;P. De Bièvre;H. Hidaka.
Journal of Physical and Chemical Reference Data (2005)
The nuclear interaction at Oklo 2 billion years ago
Yasunori Fujii;Yasunori Fujii;Akira Iwamoto;Tokio Fukahori;Toshihiko Ohnuki.
Nuclear Physics (2000)
4.2 Ga zircon xenocryst in an Acasta gneiss from northwestern Canada : Evidence for early continental crust
Tsuyoshi Iizuka;Kenji Horie;Tsuyoshi Komiya;Shigenori Maruyama.
U-Pb geochronology and REE geochemistry of zircons from Palaeoproterozoic paragneiss clasts in the Mesozoic Kamiaso conglomerate, central Japan: evidence for an Archean provenance
Hiroshi Hidaka;Hiroshi Shimizu;Mamoru Adachi.
Chemical Geology (2002)
ATOMIC WEIGHTS OF THE ELEMENTS: REVIEW 2000
Isotopic Abundances;J. R. De Laeter;J. K. Böhlke;P. De Bièvre.
Biphasic Effect of Estrogen on Neuronal Constitutive Nitric Oxide Synthase via Ca2+-Calmodulin Dependent Mechanism
T. Hayashi;T. Ishikawa;K. Yamada;M. Kuzuya.
Biochemical and Biophysical Research Communications (1994)
ION MICROPROBE U-PB DATING OF APATITE
Yuji Sano;Takayuki Oyama;Kentaro Terada;Hiroshi Hidaka.
Chemical Geology (1999)
Water Formation through a Quantum Tunneling Surface Reaction, OH + H2, at 10 K
Y. Oba;N. Watanabe;T. Hama;K. Kuwahata.
The Astrophysical Journal (2012)
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