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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

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Reference TypeJournal (article/letter/editorial)
TitleTwo-stage evolution of the Earth's mantle inferred from numerical simulation of coupled magmatism-mantle convection system with tectonic plates
JournalJournal of Geophysical Research: Solid Earth
AuthorsOgawa, MasakiAuthor
Year2014 (March)Volume119
Issue3
PublisherAmerican Geophysical Union (AGU)
DOIdoi:10.1002/2013jb010315Search in ResearchGate
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Mindat Ref. ID930212Long-form Identifiermindat:1:5:930212:3
GUID0
Full ReferenceOgawa, 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
Plain TextOgawa, 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
In(2014, March) Journal of Geophysical Research: Solid Earth Vol. 119 (3) American Geophysical Union (AGU)

See Also

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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, 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 (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, 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 (1994) Effects of chemical fractionation of heat-producing elements on mantle evolution inferred from a numerical model of coupled magmatism-mantle convection system. Physics of the Earth and Planetary Interiors, 83 (2). 101-127 doi:10.1016/0031-9201(94)90067-1
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 (2007) Superplumes, plates, and mantle magmatism in two-dimensional numerical models. Journal of Geophysical Research, 112. doi:10.1029/2006jb004533
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
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 (1997) A bifurcation in the coupled magmatism-mantle convection system and its implications for the evolution of the Earth's upper mantle. Physics of the Earth and Planetary Interiors, 102 (3). 259-276 doi:10.1016/s0031-9201(96)03244-x
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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