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Origin of Earth’s oceans: An assessment of the total amount, history and supply of water

GEOCHEMICAL JOURNAL, 2016, Vol.50(1), pp.27-42

Genda, Hidenori

2016

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Effects of Friction and Plastic Deformation in Shock‐Comminuted Damaged Rocks on Impact Heating

Geophysical research letters, 2018-01, Vol.45 (2), p.620-626

2018

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Emergence of two types of terrestrial planet on solidification of magma ocean

Nature (London), 2013-05, Vol.497 (7451), p.607-610

2013

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Escape and Accretion by Cratering Impacts: Formulation of Scaling Relations for High-speed Ejecta

The Astrophysical journal, 2020-07, Vol.898 (1), p.30

2020

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Large planets may not form fractionally large moons

Nature communications, 2022-02, Vol.13 (1), p.568-568, Article 568

2022

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Fates of hydrous materials during planetesimal collisions

Icarus (New York, N.Y. 1962), 2019-08, Vol.328, p.58-68

2019

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Numerous chondritic impactors and oxidized magma ocean set Earth’s volatile depletion

Scientific reports, 2021-10, Vol.11 (1), p.20894-20894, Article 20894

2021

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Erosion and Accretion by Cratering Impacts on Rocky and Icy Bodies

The Astrophysical journal, 2021-06, Vol.913 (2), p.77

2021

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The Role of Post‐Shock Heating by Plastic Deformation During Impact Devolatilization of Calcite (CaCO3)

Geophysical research letters, 2021-04, Vol.48 (7), p.n/a

2021

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Impact degassing and atmospheric erosion on Venus, Earth, and Mars during the late accretion

Icarus (New York, N.Y. 1962), 2019-01, Vol.317, p.48-58

2019

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Formation of Terrestrial Planets from Protoplanets Under a Realistic Accretion Condition

Astrophysical journal. Letters, 2010-05, Vol.714 (1), p.L21-L25

2010

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Implantation of Martian Materials in the Inner Solar System by a Mega Impact on Mars

Astrophysical journal. Letters, 2018-04, Vol.856 (2), p.L36

2018

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On the Impact Origin of Phobos and Deimos. I. Thermodynamic and Physical Aspects

The Astrophysical journal, 2017-08, Vol.845 (2), p.125

2017

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Hydrocode modeling of the spallation process during hypervelocity impacts: Implications for the ejection of Martian meteorites

Icarus (New York, N.Y. 1962), 2018-02, Vol.301, p.219-234

2018

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Giant impact onto a Vesta-like asteroid and formation of mesosiderites through mixing of metallic core and surface crust

Icarus (New York, N.Y. 1962), 2022-06, Vol.379, p.114949, Article 114949

2022

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Modification of the composition and density of Mercury from late accretion

Icarus (New York, N.Y. 1962), 2021-01, Vol.354, p.114064, Article 114064

2021

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Tidal Evolution of the Eccentric Moon around Dwarf Planet (225088) Gonggong

The Astronomical journal, 2021-12, Vol.162 (6), p.226

2021

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Ejection of iron-bearing giant-impact fragments and the dynamical and geochemical influence of the fragment re-accretion

Earth and planetary science letters, 2017-07, Vol.470, p.87-95

2017

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Formation of Phobos and Deimos via a giant impact

Icarus (New York, N.Y. 1962), 2015-05, Vol.252, p.334-338

2015

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Ring formation around giant planets by tidal disruption of a single passing large Kuiper belt object

Icarus (New York, N.Y. 1962), 2017-01, Vol.282, p.195-213

2017

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SPH simulations for shape deformation of rubble-pile asteroids through spinup: The challenge for making top-shaped asteroids Ryugu and Bennu

Icarus (New York, N.Y. 1962), 2021-09, Vol.365, p.114505, Article 114505

2021

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On the Impact Origin of Phobos and Deimos. II. True Polar Wander and Disk Evolution

The Astrophysical journal, 2017-12, Vol.851 (2), p.122

2017

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Transport of impact ejecta from Mars to its moons as a means to reveal Martian history

Scientific reports, 2019-12, Vol.9 (1), p.19833-6, Article 19833

2019

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Special issue “Martian Moons eXploration: the scientific investigations of Mars and its moons”

Earth, planets, and space, 2024-12, Vol.76 (1), p.8-2, Article 8

2024

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Impact erosion model for gravity-dominated planetesimals

Icarus (New York, N.Y. 1962), 2017-09, Vol.294, p.234-246

2017

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Origin of Earth’s oceans: An assessment of the total amount, history and supply of water

Effects of Friction and Plastic Deformation in Shock‐Comminuted Damaged Rocks on Impact Heating

Emergence of two types of terrestrial planet on solidification of magma ocean

Escape and Accretion by Cratering Impacts: Formulation of Scaling Relations for High-speed Ejecta

Large planets may not form fractionally large moons

Fates of hydrous materials during planetesimal collisions

Numerous chondritic impactors and oxidized magma ocean set Earth’s volatile depletion

Erosion and Accretion by Cratering Impacts on Rocky and Icy Bodies

The Role of Post‐Shock Heating by Plastic Deformation During Impact Devolatilization of Calcite (CaCO3)

Impact degassing and atmospheric erosion on Venus, Earth, and Mars during the late accretion

Formation of Terrestrial Planets from Protoplanets Under a Realistic Accretion Condition

Implantation of Martian Materials in the Inner Solar System by a Mega Impact on Mars

On the Impact Origin of Phobos and Deimos. I. Thermodynamic and Physical Aspects

Hydrocode modeling of the spallation process during hypervelocity impacts: Implications for the ejection of Martian meteorites

Giant impact onto a Vesta-like asteroid and formation of mesosiderites through mixing of metallic core and surface crust

Modification of the composition and density of Mercury from late accretion

Tidal Evolution of the Eccentric Moon around Dwarf Planet (225088) Gonggong

Ejection of iron-bearing giant-impact fragments and the dynamical and geochemical influence of the fragment re-accretion

Formation of Phobos and Deimos via a giant impact

Ring formation around giant planets by tidal disruption of a single passing large Kuiper belt object

SPH simulations for shape deformation of rubble-pile asteroids through spinup: The challenge for making top-shaped asteroids Ryugu and Bennu

On the Impact Origin of Phobos and Deimos. II. True Polar Wander and Disk Evolution

Transport of impact ejecta from Mars to its moons as a means to reveal Martian history

Special issue “Martian Moons eXploration: the scientific investigations of Mars and its moons”

Impact erosion model for gravity-dominated planetesimals

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