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Ogawa, Masaki, Yanagisawa, Takatoshi (2011) Numerical models of Martian mantle evolution induced by magmatism and solid-state convection beneath stagnant lithosphere. Journal of Geophysical Research, 116. doi:10.1029/2010je003777

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Reference TypeJournal (article/letter/editorial)
TitleNumerical models of Martian mantle evolution induced by magmatism and solid-state convection beneath stagnant lithosphere
JournalJournal of Geophysical Research
AuthorsOgawa, MasakiAuthor
Yanagisawa, TakatoshiAuthor
Year2011 (August 25)Volume116
PublisherAmerican Geophysical Union (AGU)
DOIdoi:10.1029/2010je003777Search in ResearchGate
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Mindat Ref. ID887375Long-form Identifiermindat:1:5:887375:4
GUID0
Full ReferenceOgawa, Masaki, Yanagisawa, Takatoshi (2011) Numerical models of Martian mantle evolution induced by magmatism and solid-state convection beneath stagnant lithosphere. Journal of Geophysical Research, 116. doi:10.1029/2010je003777
Plain TextOgawa, Masaki, Yanagisawa, Takatoshi (2011) Numerical models of Martian mantle evolution induced by magmatism and solid-state convection beneath stagnant lithosphere. Journal of Geophysical Research, 116. doi:10.1029/2010je003777
In(2011) Journal of Geophysical Research Vol. 116. American Geophysical Union (AGU)

See Also

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Ogawa, Masaki, Yanagisawa, Takatoshi (2012) Two-dimensional numerical studies on the effects of water on Martian mantle evolution induced by magmatism and solid-state mantle convection. Journal of Geophysical Research: Planets, 117. doi:10.1029/2012je004054
Ogawa, Masaki, Yanagisawa, Takatoshi (2014) Mantle evolution in Venus due to magmatism and phase transitions: From punctuated layered convection to whole-mantle convection. Journal of Geophysical Research: Planets, 119 (4) 867-883 doi:10.1002/2013je004593
Ogawa, Masaki (1988) Numerical experiments on coupled magmatism-mantle convection system: Implications for mantle evolution and Archean Continental Crusts. Journal of Geophysical Research: Solid Earth, 93. 15119-15134 doi:10.1029/jb093ib12p15119
Ogawa, Masaki (2021) The Four‐Stage Evolution of Martian Mantle Inferred From Numerical Simulation of the Magmatism‐Mantle Upwelling Feedback. Journal of Geophysical Research: Planets, 126 (12) doi:10.1029/2021je006997
Ogawa, Masaki (2007) Superplumes, plates, and mantle magmatism in two-dimensional numerical models. Journal of Geophysical Research, 112. doi:10.1029/2006jb004533
Ogawa, Masaki, Nakamura, Hidenori (1998) Thermochemical regime of the early mantle inferred from numerical models of the coupled magmatism-mantle convection system with the solid-solid phase transitions at depths around 660 km. Journal of Geophysical Research: Solid Earth, 103. 12161-12180 doi:10.1029/98jb00611
Ogawa, Masaki (2014) Two-stage evolution of the Earth's mantle inferred from numerical simulation of coupled magmatism-mantle convection system with tectonic plates. Journal of Geophysical Research: Solid Earth, 119 (3) 2462-2486 doi:10.1002/2013jb010315
Ogawa, Masaki (2000) Numerical models of magmatism in convecting mantle with temperature-dependent viscosity and their implications for Venus and Earth. Journal of Geophysical Research: Planets, 105. 6997-7012 doi:10.1029/1999je001162
U, Ken'yo, Kameyama, Masanori, Ogawa, Masaki (2023) The Volcanic and Radial Expansion/Contraction History of the Moon Simulated by Numerical Models of Magmatism in the Convective Mantle. Journal of Geophysical Research: Planets, 128 (9) doi:10.1029/2023je007845
Ogawa, Masaki (1993) A Numerical Model of a Coupled Magmatism—Mantle Convection System in Venus and the Earth's Mantle beneath Archean Continental Crusts. Icarus, 102 (1). 40-61 doi:10.1006/icar.1993.1031
Ogawa, Masaki (2016) Evolution of the interior of Mercury influenced by coupled magmatism-mantle convection system and heat flux from the core. Journal of Geophysical Research: Planets, 121 (2) 118-136 doi:10.1002/2015je004832
 
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