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Kazuki Takahashi

Researcher at University of Tsukuba

Publications -  28
Citations -  111

Kazuki Takahashi is an academic researcher from University of Tsukuba. The author has contributed to research in topics: Metamorphism & Nuclear reactor. The author has an hindex of 5, co-authored 23 publications receiving 67 citations. Previous affiliations of Kazuki Takahashi include New Energy and Industrial Technology Development Organization.

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Petrology, geochemistry and LA-ICP-MS U-Pb geochronology of Paleoproterozoic basement rocks in Bangladesh: An evaluation of calc-alkaline magmatism and implication for Columbia supercontinent amalgamation

TL;DR: In this paper, the pluton showed evidence of crystal fractionation involving largely plagioclase, amphibole and possibly biotite, and trace element contents also indicate the possibility of a fractionation or assimilation; explain the entire variation from diorite to monzonite, even granite.
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Investigation of the Unit-1 nuclear reactor of Fukushima Daiichi by cosmic muon radiography

TL;DR: In this paper, the status of the nuclear fuel assemblies in the Unit-1 reactor of the Fukushima Daiichi nuclear power plant by cosmic muon radiography was investigated by placing muon tracking detectors outside the reactor building.
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Investigation of Unit-1 Nuclear Reactor of the Fukushima Daiichi by Cosmic Muon Radiography

TL;DR: In this paper, the status of the nuclear fuel assemblies in Unit-1 reactor of the Fukushima Daiichi Nuclear Power plant by the method called Cosmic Muon Radiography was investigated.
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Fluid-induced high-temperature metasomatism at Rundvågshetta in the Lützow-Holm Complex, East Antarctica: Implications for the role of brine during granulite formation

TL;DR: In this paper, a petrological, phase equilibria modeling, and fluid inclusion data for pelitic and mafic granulites from Rundvagshetta in the highest-grade region of the Neoproterozoic Lutzow-Holm Complex (LHC), East Antarctica, and provide unequivocal evidence for fluid-rock interaction and high temperature metasomatism in the presence of brine fluid.