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Kenta Yoshida

Scientist (Igneous and metamorphic petrology)

Yokosuka, Japan

Publications

  • Monazite Behaviour during Metamorphic Evolution of a Diamond-bearing Gneiss
  • Fluid inclusions with high Li/B ratio in a quartz vein from the Besshi area of the Sambagawa metamorphic belt: Implications for deep geofluid evolution
  • Trace element characteristics of clinozoisite pseudomorphs after lawsonite in talc-garnet-chloritoid schists from the Makbal UHP Complex, northern Kyrgyz Tian-Shan
  • Discovery of diamond in the Tromsø Nappe, Scandinavian Caledonides (N. Norway)
  • Diamond in metasedimentary crustal rocks from Pohorje, Eastern Alps: A window to deep continental subduction
  • Microdiamond discovered in the Seve Nappe (Scandinavian Caledonides) and its exhumation by the "vacuum-cleaner" mechanism
  • Geochemical features and relative B-Li-Cl compositions of deep-origin fluids trapped in high-pressure metamorphic rocks
  • Experimental variable effects on laser heating of inclusions during Raman spectroscopic analysis
  • Multi-stage infiltration of Na- and K-rich fluids from pegmatites at mid-crustal depths as revealed by feldspar replacement textures
  • Discovery of datolite in a high–pressure marble from the Sanbagawa metamorphic belt: Indication of B–rich fluid activity
  • Metamorphism and K-Ar white mica ages of pelitic schists in the Makbal Complex, Kyrgyz Northern Tien-Shan
  • Sparse isocon analysis: A data-driven approach for material transfer estimation
  • Grain size reduction due to fracturing and subsequent grain-size-sensitive creep in a lower crustal shear zone in the presence of a CO2-bearing fluid
  • Phase relations of lawsonite-blueschists and their role as a water-budget monitor: A case study from the Hakoishi sub-unit of the Kurosegawa belt, SW Japan
  • Micro-excavation and direct chemical analysis of individual fluid inclusion by cryo-FIB-SEM-EDS: application to the UHP talc-garnet-chloritoid schist from the Makbal Metamorphic Complex, Kyrgyz Tian-Shan
  • Classification of geochemical data based on multivariate statistical analyses: Complementary roles of cluster, principal component, and independent component analyses
  • Progressive evolution of whole–rock composition during metamorphism revealed by multivariate statistical analyses
  • GEOFCM: a new method for statistical classification of geochemical data using spatial contextual information
  • Bayesian probabilistic reconstruction of metamorphic P–T paths using inclusion geothermobarometry
  • Elastic wave velocity and electrical conductivity in a brine-saturated rock and microstructure of pores
  • Monazite behaviour during metamorphic evolution of a diamond-bearing gneiss: a case study from the Seve Nappe Complex, Scandinavian Caledonides
  • Geochemical database of Japanese islands for basement rocks: compilation of domestic article
  • Recovering the past history of natural recording media by Bayesian inversion
  • A rapid and precise quantitative electron probe chemical mapping technique and its application to an ultrahigh-pressure eclogite from the Moldanubian Zone of the Bohemian Massif (Nové Dvory, Czech Republic)
  • Voyage to the west: pumice raft from the Fukutoku-Oka-no-Ba in the northwest Pacific drifted over the South China Sea to Thailand
  • Metamorphism of garnet amphibolite and pelitic schist from the Upper Unit of theMakbal Complex, Kyrgyz Northern Tian-Shan
  • Variety of the drift pumice clasts from the 2021 Fukutoku‐Oka‐no‐Ba eruption, Japan
  • Thermal structure of the Kebara Formation and its proximal areas in the western Kii Peninsula, SW Japan: Application of the carbonaceous material Raman geothermometry
  • Preiswerkite and högbomite within garnets of Aktyuz eclogite, Northern Tien Shan, Kyrgyzstan
  • Combined FIB microsampling and X-ray microtomography: A powerful tool for the study of tiny fluid inclusions
  • Grain-boundary diffusion rates inferred from grain-size variations of quartz in metacherts from a contact aureole
  • 3D chemical mapping of 'Mn-caldera shaped zoning' garnet found from the Sanbagawa metamorphic belt of the Besshi district, SW japan
  • Triassic to Early Jurassic (c. 200 Ma) UHP metamorphism in the Central Rhodopes: Evidence from U-Pb-Th dating of monazite in diamond-bearing gneiss from Chepelare (Bulgaria)
  • Annular fluid inclusions from a quartz vein intercalated with metapelites from the Besshi area of the Sanbagawa belt, SW Japan
  • Ion microprobe U-Th-Pb geochronology and study of micro-inclusions in zircon from the Himalayan high- and ultrahigh-pressure eclogites, Kaghan Valley of Pakistan
  • Petrographic characteristics in the pumice clast deposited along the Gulf of Thailand, drifted from Fukutoku-Oka-no-Ba
  • Discovery of the Early Jurassic high-temperature pre-Sanbagawa metamorphism recorded in titanite
  • Subduction-zone parameters that control slab behavior at the 660-km discontinuity revealed by logistic regression analysis and model selection
  • Decoupling of U–Pb ages and compositional zoning of garnet in a high–pressure marble from the eastern Iratsu body, Sanbagawa metamorphic terrane, Japan
  • Evolution of magma supply system beneath a submarine lava dome after the 7.3-ka caldera-forming Kikai-Akahoya eruption
  • Chocolate-chip cookie-like pumice from the 2021 Fukutoku-Oka-no-Ba eruption: views from SNS-related geology
  • The nature of the proximal volcaniclastic materials from the 2021 eruption Fukutoku-Oka-no-Ba in the Izu-Bonin arc.
  • Regression analysis and variable selection to determine the key subduction-zone parameters that determine the maximum earthquake magnitude
  • Ba stable isotope excursions induced by multiple hyperthermal events: A potential new index for transient global warming
  • Genesis and interaction of magmas at Nishinoshima volcano in the Ogasawara arc, western Pacific: new insights from submarine deposits of the 2020 explosive eruptions
  • Oxidation-induced nanolite crystallization triggered the 2021 eruption of Fukutoku-Oka-no-Ba, Japan
  • 鬼界カルデラ噴火の総合理解に向けた噴出物化学組成データベースの構築
  • The proximal volcaniclastic materials of Fukutoku‐Oka‐no‐Ba in the Izu‐Bonin arc show contrasting characteristics to the drift pumice of the 2021 eruption
  • Rock magnetic analyses as a tool to investigate diversity of drift pumice clasts: An example from Japan's 2021 Fukutoku‐Oka‐no‐Ba (FOB) eruption
  • The Sofu Seamount Present in the Source Area of the October 2023 Earthquake and Tsunami in Japan

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