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Experimental Hydrothermal Alteration of Rhyolite and Andesite at 325 °C and 300 Bar: Implications for a Potential Role of Volcanic Glass in the Fluid Composition in the Okinawa Trough.
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- Minerals (2075-163X), 2024, v. 14, n. 3, p. 259, doi. 10.3390/min14030259
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- Article
Mineralogical alteration of a type A CAI from Allende CV3 chondrite: Formation of secondary dmisteinbergite and its phase transition to anorthite.
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- Meteoritics & Planetary Science, 2023, v. 58, n. 3, p. 405, doi. 10.1111/maps.13961
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- Article
Liquid and supercritical CO<sub>2</sub> as an organic solvent in Hadean seafloor hydrothermal systems: implications for prebiotic chemical evolution.
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- Progress in Earth & Planetary Science, 2022, v. 9, n. 1, p. 1, doi. 10.1186/s40645-022-00510-6
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Chemical Nature of Hydrothermal Fluids Generated by Serpentinization and Carbonation of Komatiite: Implications for H<sub>2</sub>‐Rich Hydrothermal System and Ocean Chemistry in the Early Earth.
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- Geochemistry, Geophysics, Geosystems: G3, 2021, v. 22, n. 12, p. 1, doi. 10.1029/2021GC009827
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Organic matter in carbonaceous chondrite lithologies of Almahata Sitta: Incorporation of previously unsampled carbonaceous chondrite lithologies into ureilitic regolith.
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- Meteoritics & Planetary Science, 2021, v. 56, n. 7, p. 1311, doi. 10.1111/maps.13713
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Thermodynamic Constraints on Smectite and Iron Oxide Formation at Gale Crater, Mars: Insights into Potential Free Energy from Aerobic Fe Oxidation in Lake Water–Groundwater Mixing Zone.
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- Minerals (2075-163X), 2021, v. 11, n. 4, p. 341, doi. 10.3390/min11040341
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Composition of the Primordial Ocean Just after Its Formation: Constraints from the Reactions between the Primitive Crust and a Strongly Acidic, CO 2 -Rich Fluid at Elevated Temperatures and Pressures.
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- Minerals (2075-163X), 2021, v. 11, n. 4, p. 389, doi. 10.3390/min11040389
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Stable Abiotic Production of Ammonia from Nitrate in Komatiite-Hosted Hydrothermal Systems in the Hadean and Archean Oceans.
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- Minerals (2075-163X), 2021, v. 11, n. 3, p. 321, doi. 10.3390/min11030321
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Experimental Simulations of Hypervelocity Impact Penetration of Asteroids Into the Terrestrial Ocean and Benthic Cratering.
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- Journal of Geophysical Research. Planets, 2020, v. 125, n. 12, p. 1, doi. 10.1029/2019JE006291
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Kinetics in thermal evolution of Raman spectra of chondritic organic matter to evaluate thermal history of their parent bodies.
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- Meteoritics & Planetary Science, 2020, v. 55, n. 8, p. 1, doi. 10.1111/maps.13548
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Chemical assessment of the explosive chamber in the projector system of Hayabusa2 for asteroid sampling.
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- Earth, Planets & Space, 2020, v. 72, n. 1, p. 1, doi. 10.1186/s40623-020-01217-y
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Genome‐enabled metabolic reconstruction of dominant chemosynthetic colonizers in deep‐sea massive sulfide deposits.
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- Environmental Microbiology, 2018, v. 20, n. 2, p. 862, doi. 10.1111/1462-2920.14032
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Weak hydrothermal carbonation of the Ongeluk volcanics: evidence for low CO concentrations in seawater and atmosphere during the Paleoproterozoic global glaciation.
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- Progress in Earth & Planetary Science, 2017, v. 4, n. 1, p. 1, doi. 10.1186/s40645-017-0145-6
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- Article
Reactions between komatiite and CO-rich seawater at 250 and 350 °C, 500 bars: implications for hydrogen generation in the Hadean seafloor hydrothermal system.
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- Progress in Earth & Planetary Science, 2016, v. 3, n. 1, p. 1, doi. 10.1186/s40645-016-0111-8
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Rapid growth of mineral deposits at artificial seafloor hydrothermal vents.
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- Scientific Reports, 2016, p. 22163, doi. 10.1038/srep22163
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Hydrogen-rich hydrothermal environments in the Hadean ocean inferred from serpentinization of komatiites at 300 °C and 500 bar.
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- Progress in Earth & Planetary Science, 2015, v. 2, n. 1, p. 1, doi. 10.1186/s40645-015-0076-z
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Authigenic carbonate precipitation at the end-Guadalupian (Middle Permian) in China: Implications for the carbon cycle in ancient anoxic oceans.
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- Progress in Earth & Planetary Science, 2015, v. 2, n. 1, p. 1, doi. 10.1186/s40645-015-0073-2
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High-temperature water-rock interactions and hydrothermal environments in the chondrite-like core of Enceladus.
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- Nature Communications, 2015, v. 6, n. 10, p. 8604, doi. 10.1038/ncomms9604
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Potential for biogeochemical cycling of sulfur, iron and carbon within massive sulfide deposits below the seafloor.
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- Environmental Microbiology, 2015, v. 17, n. 5, p. 1817, doi. 10.1111/1462-2920.12648
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Ongoing hydrothermal activities within Enceladus.
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- Nature, 2015, v. 519, n. 7542, p. 207, doi. 10.1038/nature14262
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Rock magnetism of tiny exsolved magnetite in plagioclase from a Paleoarchean granitoid in the Pilbara craton.
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- Geochemistry, Geophysics, Geosystems: G3, 2015, v. 16, n. 1, p. 112, doi. 10.1002/2014GC005508
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Exploration of Enceladus' Water-Rich Plumes toward Understanding of Chemistry and Biology of the Interior Ocean.
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- Transactions of the Japan Society of Aeronautical & Space Sciences, Aerospace Technology Japan, 2014, v. 12, n. ists 29, p. 7
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Post-drilling changes in fluid discharge pattern, mineral deposition, and fluid chemistry in the Iheya North hydrothermal field, Okinawa Trough.
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- Geochemistry, Geophysics, Geosystems: G3, 2013, v. 14, n. 11, p. 4774, doi. 10.1002/2013GC004895
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Discovery of New Hydrothermal Activity and Chemosynthetic Fauna on the Central Indian Ridge at 18°-20°S.
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- PLoS ONE, 2012, v. 7, n. 3, p. 1, doi. 10.1371/journal.pone.0032965
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Monazite geochronology and geochemistry of meta-sediments in the Narryer Gneiss Complex, Western Australia: constraints on the tectonothermal history and provenance.
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- Contributions to Mineralogy & Petrology, 2010, v. 160, n. 6, p. 803, doi. 10.1007/s00410-010-0508-0
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