메뉴 건너뛰기




Volumn 215, Issue 1, 2011, Pages 346-357

Origin of the martian dichotomy and Tharsis from a giant impact causing massive magmatism

Author keywords

Geophysics; Mars; Planetary dynamics; Planetary formation

Indexed keywords


EID: 80052030257     PISSN: 00191035     EISSN: 10902643     Source Type: Journal    
DOI: 10.1016/j.icarus.2011.06.012     Document Type: Article
Times cited : (78)

References (87)
  • 1
    • 46249109227 scopus 로고    scopus 로고
    • The Borealis basin and the origin of the martian crustal dichotomy
    • Andrews-Hanna J.C., Zuber M.T., Banerdt W.B. The Borealis basin and the origin of the martian crustal dichotomy. Nature 2008, 453:1212-1215.
    • (2008) Nature , vol.453 , pp. 1212-1215
    • Andrews-Hanna, J.C.1    Zuber, M.T.2    Banerdt, W.B.3
  • 2
    • 0030955379 scopus 로고    scopus 로고
    • Mineralogy of the martian interior up to core-mantle boundary pressures
    • Bertka C.M., Fei Y. Mineralogy of the martian interior up to core-mantle boundary pressures. J. Geophys. Res. 1997, 102:5251-5264.
    • (1997) J. Geophys. Res. , vol.102 , pp. 5251-5264
    • Bertka, C.M.1    Fei, Y.2
  • 3
    • 0000886183 scopus 로고
    • The viscosity of magmatic silicate liquids: A model for calculation
    • Bottinga Y., Weill D.F. The viscosity of magmatic silicate liquids: A model for calculation. Am. J. Sci. 1972, 272:438-475.
    • (1972) Am. J. Sci. , vol.272 , pp. 438-475
    • Bottinga, Y.1    Weill, D.F.2
  • 4
    • 31444452623 scopus 로고    scopus 로고
    • Viscosity of the martian mantle and its initial temperature: Constraints from crust formation history and the evolution of the magnetic field
    • Breuer D., Spohn T. Viscosity of the martian mantle and its initial temperature: Constraints from crust formation history and the evolution of the magnetic field. Planet. Space Sci. 2006, 54:153-169.
    • (2006) Planet. Space Sci. , vol.54 , pp. 153-169
    • Breuer, D.1    Spohn, T.2
  • 5
    • 80052029301 scopus 로고    scopus 로고
    • Taschenbuch der Mathematik, fifth ed., Harri Deutsch, Frankfurt am Main
    • Bronstein, I.N., Semendjajew, K.A., Musiol, G., Mühlig, H. 2001. Taschenbuch der Mathematik, fifth ed., Harri Deutsch, Frankfurt am Main, 1191pp.
    • (2001) , pp. 1191
    • Bronstein, I.N.1    Semendjajew, K.A.2    Musiol, G.3    Mühlig, H.4
  • 6
    • 14844351064 scopus 로고    scopus 로고
    • The role of viscous heating in Barrovian metamorphism of collisional orogens: Thermomechanical models and application to the Lepontine Dome in the Central Alps
    • Burg J.-P., Gerya T.V. The role of viscous heating in Barrovian metamorphism of collisional orogens: Thermomechanical models and application to the Lepontine Dome in the Central Alps. J. Metamorp. Geol. 2005, 23:75-95.
    • (2005) J. Metamorp. Geol. , vol.23 , pp. 75-95
    • Burg, J.-P.1    Gerya, T.V.2
  • 8
    • 0002269256 scopus 로고
    • Earth and Mars: Water inventories as clues to accretional histories
    • Carr M.H., Wänke H. Earth and Mars: Water inventories as clues to accretional histories. Icarus 1992, 98:61-71.
    • (1992) Icarus , vol.98 , pp. 61-71
    • Carr, M.H.1    Wänke, H.2
  • 9
    • 0000049976 scopus 로고    scopus 로고
    • Making the terrestrial planets: N-body integrations of planetary embryos in three dimensions
    • Chambers J.E., Wetherill G.W. Making the terrestrial planets: N-body integrations of planetary embryos in three dimensions. Icarus 1998, 136:304-327.
    • (1998) Icarus , vol.136 , pp. 304-327
    • Chambers, J.E.1    Wetherill, G.W.2
  • 10
    • 22144460994 scopus 로고    scopus 로고
    • Computation of phase equilibria by linear programming: A tool for geodynamic modeling and its application to subduction zone decarbonation
    • Connolly J.A.D. Computation of phase equilibria by linear programming: A tool for geodynamic modeling and its application to subduction zone decarbonation. Earth Planet. Sci. Lett. 2005, 236:524-541.
    • (2005) Earth Planet. Sci. Lett. , vol.236 , pp. 524-541
    • Connolly, J.A.D.1
  • 11
    • 0020387096 scopus 로고
    • A first-order estimate of shock heating and vaporization in oceanic impacts
    • Geological implications of impacts of large asteroids and comets on Earth
    • Croft S.K. A first-order estimate of shock heating and vaporization in oceanic impacts. Spec. Pap. Geol. Soc. Am. 1982, 190:143-152.
    • (1982) Spec. Pap. Geol. Soc. Am. , vol.190 , pp. 143-152
    • Croft, S.K.1
  • 12
    • 77953027943 scopus 로고    scopus 로고
    • Turbulent mixing of metal and silicate during planet accretion - And interpretation of the Hf-W chronometer
    • Dahl T.W., Stevenson D.J. Turbulent mixing of metal and silicate during planet accretion - And interpretation of the Hf-W chronometer. Earth Planet. Sci. Lett. 2010, 295:177-186.
    • (2010) Earth Planet. Sci. Lett. , vol.295 , pp. 177-186
    • Dahl, T.W.1    Stevenson, D.J.2
  • 13
    • 77954626407 scopus 로고    scopus 로고
    • Temperature and heat flux scalings for isoviscous thermal convection in spherical geometry
    • Deschamps F., Tackley P.J., Nakagawa T. Temperature and heat flux scalings for isoviscous thermal convection in spherical geometry. Geophys. J. Int. 2010, 182:137-154.
    • (2010) Geophys. J. Int. , vol.182 , pp. 137-154
    • Deschamps, F.1    Tackley, P.J.2    Nakagawa, T.3
  • 14
    • 0000878746 scopus 로고
    • Thaumasia: A fossilized early forming Tharsis uplift
    • Frey H.V. Thaumasia: A fossilized early forming Tharsis uplift. J. Geophys. Res. 1979, 84:1009-1023.
    • (1979) J. Geophys. Res. , vol.84 , pp. 1009-1023
    • Frey, H.V.1
  • 15
    • 33745442806 scopus 로고    scopus 로고
    • Impact constraints on the age and origin of the lowlands of Mars
    • Frey H.V. Impact constraints on the age and origin of the lowlands of Mars. Geophys. Res. Lett. 2006, 33:L08S02.
    • (2006) Geophys. Res. Lett. , vol.33
    • Frey, H.V.1
  • 16
    • 0023774859 scopus 로고
    • Large impact basins and the mega-impact origin for the crustal dichotomy on Mars
    • Frey H., Schultz R.A. Large impact basins and the mega-impact origin for the crustal dichotomy on Mars. Geophys. Res. Lett. 1988, 15:229-232.
    • (1988) Geophys. Res. Lett. , vol.15 , pp. 229-232
    • Frey, H.1    Schultz, R.A.2
  • 17
    • 34547870142 scopus 로고    scopus 로고
    • Robust characteristics method for modelling multiphase visco-elasto-plastic thermo-mechanical problems
    • Gerya T.V., Yuen D.A. Robust characteristics method for modelling multiphase visco-elasto-plastic thermo-mechanical problems. Phys. Earth Planet. Int. 2007, 163:83-105.
    • (2007) Phys. Earth Planet. Int. , vol.163 , pp. 83-105
    • Gerya, T.V.1    Yuen, D.A.2
  • 18
    • 0000802370 scopus 로고    scopus 로고
    • A thermal model for the differentiation of asteroid 4 vesta, based on radiogenic heating
    • Ghosh A., McSween H.Y. A thermal model for the differentiation of asteroid 4 vesta, based on radiogenic heating. Icarus 1998, 134:187-206.
    • (1998) Icarus , vol.134 , pp. 187-206
    • Ghosh, A.1    McSween, H.Y.2
  • 20
    • 0027446808 scopus 로고
    • Effects of surface cooling on the spreading of lava flows and domes
    • Griffiths R.W., Fink J.H. Effects of surface cooling on the spreading of lava flows and domes. J. Fluid Mech. 1993, 252:667-702.
    • (1993) J. Fluid Mech. , vol.252 , pp. 667-702
    • Griffiths, R.W.1    Fink, J.H.2
  • 21
    • 84871802961 scopus 로고    scopus 로고
    • On the spatial variability of the martian elastic lithosphere thickness: Evidence for mantle plumes?
    • Grott M., Breuer D. On the spatial variability of the martian elastic lithosphere thickness: Evidence for mantle plumes?. J. Geophys. Res. 2010, 115:E03005.
    • (2010) J. Geophys. Res. , vol.115
    • Grott, M.1    Breuer, D.2
  • 22
    • 0029728852 scopus 로고    scopus 로고
    • A one-plume model of martian mantle convection
    • Harder H., Christensen U.R. A one-plume model of martian mantle convection. Nature 1996, 380:507-509.
    • (1996) Nature , vol.380 , pp. 507-509
    • Harder, H.1    Christensen, U.R.2
  • 23
  • 24
    • 0037173901 scopus 로고    scopus 로고
    • Thermal and crustal evolution of Mars
    • Hauck S.A., Phillips R.J. Thermal and crustal evolution of Mars. J. Geophys. Res. 2002, 107:5052.
    • (2002) J. Geophys. Res. , vol.107 , pp. 5052
    • Hauck, S.A.1    Phillips, R.J.2
  • 25
    • 55749094026 scopus 로고    scopus 로고
    • Modeling mantle convection in the spherical annulus
    • Hernlund J.W., Tackley P.J. Modeling mantle convection in the spherical annulus. Phys. Earth Planet. Int. 2008, 171:48-54.
    • (2008) Phys. Earth Planet. Int. , vol.171 , pp. 48-54
    • Hernlund, J.W.1    Tackley, P.J.2
  • 26
    • 84910026251 scopus 로고    scopus 로고
    • Mantle solidus: Experimental constraints and the effects of peridotite composition
    • 2000GC000070
    • Hirschmann M.M. Mantle solidus: Experimental constraints and the effects of peridotite composition. Geochem. Geophys. Geosyst. 2000, 1. 2000GC000070.
    • (2000) Geochem. Geophys. Geosyst. , vol.1
    • Hirschmann, M.M.1
  • 27
    • 70349925301 scopus 로고    scopus 로고
    • Coupled core-mantle thermal evolution of early Mars
    • Ke Y., Solomatov V.S. Coupled core-mantle thermal evolution of early Mars. J. Geophys. Res. 2009, 114:E07004.
    • (2009) J. Geophys. Res. , vol.114
    • Ke, Y.1    Solomatov, V.S.2
  • 28
    • 67649964305 scopus 로고    scopus 로고
    • Towards self-consistent modelling of the martian dichotomy: The influence of one-ridge convection on crustal thickness distribution
    • Keller T., Tackley P.J. Towards self-consistent modelling of the martian dichotomy: The influence of one-ridge convection on crustal thickness distribution. Icarus 2009, 202:429-443.
    • (2009) Icarus , vol.202 , pp. 429-443
    • Keller, T.1    Tackley, P.J.2
  • 29
    • 55049094284 scopus 로고    scopus 로고
    • Constraining the composition and thermal state of Mars from inversion of geophysical data
    • Khan A., Connolly J.A.D. Constraining the composition and thermal state of Mars from inversion of geophysical data. J. Geophys. Res. 2008, 113:E07003.
    • (2008) J. Geophys. Res. , vol.113
    • Khan, A.1    Connolly, J.A.D.2
  • 30
    • 1542346826 scopus 로고    scopus 로고
    • Melting in the martian mantle: Shergottite formation and implications for present-day mantle convection on Mars
    • Kiefer W.S. Melting in the martian mantle: Shergottite formation and implications for present-day mantle convection on Mars. Meteorit. Planet. Sci. 2003, 39:1815-1832.
    • (2003) Meteorit. Planet. Sci. , vol.39 , pp. 1815-1832
    • Kiefer, W.S.1
  • 31
    • 0030239593 scopus 로고    scopus 로고
    • On runaway growth of planetesimals
    • Kokubo E., Ida S. On runaway growth of planetesimals. Icarus 1996, 123:180-191.
    • (1996) Icarus , vol.123 , pp. 180-191
    • Kokubo, E.1    Ida, S.2
  • 32
    • 36849117606 scopus 로고
    • Turbulent thermal convection at arbitrary Prandtl number
    • Kraichnan R.H. Turbulent thermal convection at arbitrary Prandtl number. Phys. Fluids 1962, 5:1374-1389.
    • (1962) Phys. Fluids , vol.5 , pp. 1374-1389
    • Kraichnan, R.H.1
  • 33
    • 35948951977 scopus 로고    scopus 로고
    • Mantle convection and magma production on present-day Mars: Effects of temperature-dependent rheology
    • Li Q., Kiefer W.S. Mantle convection and magma production on present-day Mars: Effects of temperature-dependent rheology. Geophys. Res. Lett. 2007, 34:L16203.
    • (2007) Geophys. Res. Lett. , vol.34
    • Li, Q.1    Kiefer, W.S.2
  • 35
    • 70350622864 scopus 로고    scopus 로고
    • Numerical modeling of protocore destabilization during planetary accretion: Methodology and results
    • Lin J.-R., Gerya T.V., Tackley P.J., Yuen D.A., Golabek G.J. Numerical modeling of protocore destabilization during planetary accretion: Methodology and results. Icarus 2009, 204:732-748.
    • (2009) Icarus , vol.204 , pp. 732-748
    • Lin, J.-R.1    Gerya, T.V.2    Tackley, P.J.3    Yuen, D.A.4    Golabek, G.J.5
  • 36
    • 0031124070 scopus 로고    scopus 로고
    • An oxygen isotope model for the composition of Mars
    • Lodders K., Fegley B. An oxygen isotope model for the composition of Mars. Icarus 1997, 126:373-394.
    • (1997) Icarus , vol.126 , pp. 373-394
    • Lodders, K.1    Fegley, B.2
  • 38
    • 0026269652 scopus 로고
    • High-temperature rheology of enstatite: Implications for creep in the mantle
    • Mackwell S.J. High-temperature rheology of enstatite: Implications for creep in the mantle. Geophys. Res. Lett. 1991, 18:2027-2030.
    • (1991) Geophys. Res. Lett. , vol.18 , pp. 2027-2030
    • Mackwell, S.J.1
  • 39
    • 46249127759 scopus 로고    scopus 로고
    • Mega-impact formation of the Mars hemispheric dichotomy
    • Marinova M.M., Aharonson O., Asphaug E. Mega-impact formation of the Mars hemispheric dichotomy. Nature 2008, 453:1216-1219.
    • (2008) Nature , vol.453 , pp. 1216-1219
    • Marinova, M.M.1    Aharonson, O.2    Asphaug, E.3
  • 41
    • 44349094590 scopus 로고
    • The volume and composition of melt generated by extension of the lithosphere
    • McKenzie D., Bickle M.J. The volume and composition of melt generated by extension of the lithosphere. J. Petrol. 1988, 29:625-679.
    • (1988) J. Petrol. , vol.29 , pp. 625-679
    • McKenzie, D.1    Bickle, M.J.2
  • 42
    • 0025628318 scopus 로고
    • The strength of mantle silicates at high pressures and room temperature: Implications for the viscosity of the mantle
    • Meade C., Jeanloz R. The strength of mantle silicates at high pressures and room temperature: Implications for the viscosity of the mantle. Nature 1990, 348:533-535.
    • (1990) Nature , vol.348 , pp. 533-535
    • Meade, C.1    Jeanloz, R.2
  • 44
    • 19944391283 scopus 로고    scopus 로고
    • Recent and episodic volcanic and glacial activity on Mars revealed by the High Resolution Stereo Camera
    • Neukum G., et al. Recent and episodic volcanic and glacial activity on Mars revealed by the High Resolution Stereo Camera. Nature 2004, 432:971-979.
    • (2004) Nature , vol.432 , pp. 971-979
    • Neukum, G.1
  • 46
    • 77956530124 scopus 로고    scopus 로고
    • Stable isotope measurements of martian atmospheric CO2 at the phoenix landing site
    • Niles P.B., Boynton W.V., Hoffman J.H., Ming D.W., Hamara D. Stable isotope measurements of martian atmospheric CO2 at the phoenix landing site. Science 2010, 329:1334-1337.
    • (2010) Science , vol.329 , pp. 1334-1337
    • Niles, P.B.1    Boynton, W.V.2    Hoffman, J.H.3    Ming, D.W.4    Hamara, D.5
  • 47
    • 35448931904 scopus 로고    scopus 로고
    • How rapidly did Mars accrete? Uncertainties in the Hf-W timing of core formation
    • Nimmo F., Kleine T. How rapidly did Mars accrete? Uncertainties in the Hf-W timing of core formation. Icarus 2007, 191:497-504.
    • (2007) Icarus , vol.191 , pp. 497-504
    • Nimmo, F.1    Kleine, T.2
  • 49
    • 46249126029 scopus 로고    scopus 로고
    • Implications of an impact origin for the martian hemispheric dichotomy
    • Nimmo F., Hart S.D., Korycansky D.G., Agnor C.B. Implications of an impact origin for the martian hemispheric dichotomy. Nature 2008, 453:1220-1223.
    • (2008) Nature , vol.453 , pp. 1220-1223
    • Nimmo, F.1    Hart, S.D.2    Korycansky, D.G.3    Agnor, C.B.4
  • 50
    • 0033134068 scopus 로고    scopus 로고
    • The composition and thickness of the crust of Mars estimated from rare Earth elements and neodymium-isotopic compositions of martian meteorites
    • Norman M.D. The composition and thickness of the crust of Mars estimated from rare Earth elements and neodymium-isotopic compositions of martian meteorites. Meteorit. Planet. Sci. 1999, 34:439-449.
    • (1999) Meteorit. Planet. Sci. , vol.34 , pp. 439-449
    • Norman, M.D.1
  • 51
    • 0001392775 scopus 로고
    • Impact-induced energy partitioning, melting, and vaporization on terrestrial planets
    • O'Keefe J.D., Ahrens T.J. Impact-induced energy partitioning, melting, and vaporization on terrestrial planets. Proc. Lunar Sci. Conf. 1977, 8:3357-3374.
    • (1977) Proc. Lunar Sci. Conf. , vol.8 , pp. 3357-3374
    • O'Keefe, J.D.1    Ahrens, T.J.2
  • 52
    • 34548667225 scopus 로고    scopus 로고
    • Melt propagation and volcanism in mantle convection simulations, with application for martian volcanic and atmospheric evolution
    • O'Neill C., Lenardic A., Jellinek A.M., Kiefer W.S. Melt propagation and volcanism in mantle convection simulations, with application for martian volcanic and atmospheric evolution. J. Geophys. Res. 2007, 112:E07003.
    • (2007) J. Geophys. Res. , vol.112
    • O'Neill, C.1    Lenardic, A.2    Jellinek, A.M.3    Kiefer, W.S.4
  • 53
    • 0035970864 scopus 로고    scopus 로고
    • Ancient geodynamics and global-scale hydrology on Mars
    • Phillips R.J., et al. Ancient geodynamics and global-scale hydrology on Mars. Science 2001, 291:2587-2591.
    • (2001) Science , vol.291 , pp. 2587-2591
    • Phillips, R.J.1
  • 54
    • 0027047749 scopus 로고
    • Methods of determining the rheological properties of magmas at subliquidus temperatures, J
    • Pinkerton H., Stevenson R.J. Methods of determining the rheological properties of magmas at subliquidus temperatures, J. Volcanol. Geotherm. Res. 1992, 53:47-66.
    • (1992) Volcanol. Geotherm. Res. , vol.53 , pp. 47-66
    • Pinkerton, H.1    Stevenson, R.J.2
  • 55
    • 0004294404 scopus 로고
    • Chapman & Hall, London, UK
    • Ranalli G. Rheology of the Earth 1995, Chapman & Hall, London, UK, 436pp. second ed.
    • (1995) Rheology of the Earth , pp. 436
    • Ranalli, G.1
  • 56
    • 33745875654 scopus 로고    scopus 로고
    • High resolution simulations of the final assembly of Earth-like planets I. Terrestrial accretion and dynamics
    • Raymond S.N., Quinn T., Lunine J.I. High resolution simulations of the final assembly of Earth-like planets I. Terrestrial accretion and dynamics. Icarus 2006, 183:265-282.
    • (2006) Icarus , vol.183 , pp. 265-282
    • Raymond, S.N.1    Quinn, T.2    Lunine, J.I.3
  • 57
    • 33747285854 scopus 로고    scopus 로고
    • Fluid dynamics of local martian magma oceans
    • Reese C.C., Solomatov V.S. Fluid dynamics of local martian magma oceans. Icarus 2006, 184:102-120.
    • (2006) Icarus , vol.184 , pp. 102-120
    • Reese, C.C.1    Solomatov, V.S.2
  • 58
    • 77950050166 scopus 로고    scopus 로고
    • Early martian dynamo generation due to giant impacts
    • Reese C.C., Solomatov V.S. Early martian dynamo generation due to giant impacts. Icarus 2010, 207:82-97.
    • (2010) Icarus , vol.207 , pp. 82-97
    • Reese, C.C.1    Solomatov, V.S.2
  • 59
    • 0037175293 scopus 로고    scopus 로고
    • Survival of impact-induced thermal anomalies in the martian mantle
    • Reese C.C., Solomatov V.S., Baumgardner J.R. Survival of impact-induced thermal anomalies in the martian mantle. J. Geophys. Res. 2002, 107:5082.
    • (2002) J. Geophys. Res. , vol.107 , pp. 5082
    • Reese, C.C.1    Solomatov, V.S.2    Baumgardner, J.R.3
  • 60
    • 77953083703 scopus 로고    scopus 로고
    • Impact origin for the martian crustal dichotomy: Half-emptied or half-filled? J
    • Reese C.C., Orth C.P., Solomatov V.S. Impact origin for the martian crustal dichotomy: Half-emptied or half-filled? J. Geophys. Res. 2010, 115:E05004.
    • (2010) Geophys. Res. , vol.115
    • Reese, C.C.1    Orth, C.P.2    Solomatov, V.S.3
  • 61
    • 67449098326 scopus 로고    scopus 로고
    • A multiphase model of runaway core-mantle segregation in planetary embryos
    • Ricard Y., Šrámek O., Dubuffet F. A multiphase model of runaway core-mantle segregation in planetary embryos. Earth Planet. Sci. Lett. 2009, 284:144-150.
    • (2009) Earth Planet. Sci. Lett. , vol.284 , pp. 144-150
    • Ricard, Y.1    Šrámek, O.2    Dubuffet, F.3
  • 62
    • 33750620969 scopus 로고    scopus 로고
    • Degree-1 convection in the martian mantle and the origin of the hemispheric dichotomy
    • Roberts J.H., Zhong S. Degree-1 convection in the martian mantle and the origin of the hemispheric dichotomy. J. Geophys. Res. 2006, 111:E06013.
    • (2006) J. Geophys. Res. , vol.111
    • Roberts, J.H.1    Zhong, S.2
  • 63
    • 84882929142 scopus 로고    scopus 로고
    • Formation of the Earth's core
    • Elsevier B.V., Amsterdam, Netherlands, D.J. Stevenson (Ed.) Treatise on Geophysics
    • Rubie D.C., Nimmo F., Melosh H.J. Formation of the Earth's core. Evolution of the Earth 2007, vol. 9:51-90. Elsevier B.V., Amsterdam, Netherlands. D.J. Stevenson (Ed.).
    • (2007) Evolution of the Earth , vol.9 , pp. 51-90
    • Rubie, D.C.1    Nimmo, F.2    Melosh, H.J.3
  • 64
    • 34250657687 scopus 로고    scopus 로고
    • Chondrites and the protoplanetary disk
    • Scott E.R.D. Chondrites and the protoplanetary disk. Annu. Rev. Earth Planet. Sci. 2007, 35:577-620.
    • (2007) Annu. Rev. Earth Planet. Sci. , vol.35 , pp. 577-620
    • Scott, E.R.D.1
  • 66
    • 4243254563 scopus 로고
    • High Rayleigh number convection
    • Siggia E.D. High Rayleigh number convection. Annu. Rev Fluid Mech. 1994, 26:137-168.
    • (1994) Annu. Rev Fluid Mech. , vol.26 , pp. 137-168
    • Siggia, E.D.1
  • 67
    • 84882844734 scopus 로고    scopus 로고
    • Magma oceans and primordial mantle differentiation
    • Elsevier B.V., Amsterdam, Netherlands, D.J. Stevenson (Ed.) Treatise on Geophysics
    • Solomatov V.S. Magma oceans and primordial mantle differentiation. Evolution of the Earth 2007, vol. 9:91-119. Elsevier B.V., Amsterdam, Netherlands. D.J. Stevenson (Ed.).
    • (2007) Evolution of the Earth , vol.9 , pp. 91-119
    • Solomatov, V.S.1
  • 68
    • 0000223071 scopus 로고
    • Formation, history and energetics of cores in the terrestrial planets
    • Solomon S.C. Formation, history and energetics of cores in the terrestrial planets. Phys. Earth Planet. Int. 1979, 19:168-192.
    • (1979) Phys. Earth Planet. Int. , vol.19 , pp. 168-192
    • Solomon, S.C.1
  • 69
    • 20044367442 scopus 로고    scopus 로고
    • New perspectives on ancient Mars
    • Solomon S.C., et al. New perspectives on ancient Mars. Science 2005, 307:1214-1220.
    • (2005) Science , vol.307 , pp. 1214-1220
    • Solomon, S.C.1
  • 70
    • 0033574364 scopus 로고    scopus 로고
    • Three-dimensional thermal convection in an iso-viscous, infinite Prandtl number fluid heated from within and from below: Application to the transfer of heat through planetary mantles
    • Sotin C., Labrosse S. Three-dimensional thermal convection in an iso-viscous, infinite Prandtl number fluid heated from within and from below: Application to the transfer of heat through planetary mantles. Phys. Earth Planet. Int. 1999, 112:171-190.
    • (1999) Phys. Earth Planet. Int. , vol.112 , pp. 171-190
    • Sotin, C.1    Labrosse, S.2
  • 71
    • 77957584072 scopus 로고    scopus 로고
    • Long-wavelength stagnant-lid convection with hemispheric variation in lithospheric thickness: Link between martian crustal dichotomy and Tharsis?
    • Šrámek O., Zhong S. Long-wavelength stagnant-lid convection with hemispheric variation in lithospheric thickness: Link between martian crustal dichotomy and Tharsis?. J. Geophys. Res. 2010, 115:E09010.
    • (2010) J. Geophys. Res. , vol.115
    • Šrámek, O.1    Zhong, S.2
  • 72
    • 0032522003 scopus 로고    scopus 로고
    • Density and thermal expansion of a peridotite melt at high pressure
    • Suzuki A., Ohtani E., Kato T. Density and thermal expansion of a peridotite melt at high pressure. Phys. Earth Planet. Int. 1998, 107:53-61.
    • (1998) Phys. Earth Planet. Int. , vol.107 , pp. 53-61
    • Suzuki, A.1    Ohtani, E.2    Kato, T.3
  • 73
    • 55749083087 scopus 로고    scopus 로고
    • Modelling compressible mantle convection with large viscosity contrasts in a three-dimensional spherical shell using the yin-yang grid
    • Tackley P.J. Modelling compressible mantle convection with large viscosity contrasts in a three-dimensional spherical shell using the yin-yang grid. Phys. Earth Planet. Int. 2008, 171:7-18.
    • (2008) Phys. Earth Planet. Int. , vol.171 , pp. 7-18
    • Tackley, P.J.1
  • 76
    • 38949158656 scopus 로고    scopus 로고
    • Bulk composition and early differentiation of Mars
    • Taylor G.J., et al. Bulk composition and early differentiation of Mars. J. Geophys. Res. 2006, 111:E03S10.
    • (2006) J. Geophys. Res. , vol.111
    • Taylor, G.J.1
  • 77
    • 0027456210 scopus 로고
    • Magma ocean formation due to giant impacts
    • Tonks W.B., Melosh H.J. Magma ocean formation due to giant impacts. J. Geophys. Res. 1993, 98:5319-5333.
    • (1993) J. Geophys. Res. , vol.98 , pp. 5319-5333
    • Tonks, W.B.1    Melosh, H.J.2
  • 78
    • 22144451437 scopus 로고    scopus 로고
    • Core formation and the oxidation state of the Earth
    • Wade J., Wood B.J. Core formation and the oxidation state of the Earth. Earth Planet. Sci. Lett. 2005, 236:78-95.
    • (2005) Earth Planet. Sci. Lett. , vol.236 , pp. 78-95
    • Wade, J.1    Wood, B.J.2
  • 79
    • 0028259780 scopus 로고
    • Diapiric ascent of magmas through power law crust and mantle
    • Weinberg R.F., Podladchikov Y. Diapiric ascent of magmas through power law crust and mantle. J. Geophys. Res. 1994, 99:9543-9559.
    • (1994) J. Geophys. Res. , vol.99 , pp. 9543-9559
    • Weinberg, R.F.1    Podladchikov, Y.2
  • 80
    • 0029472589 scopus 로고
    • The effects of a deep mantle endothermic phase change on the structure of thermal convection in silicate planets
    • Weinstein S.A. The effects of a deep mantle endothermic phase change on the structure of thermal convection in silicate planets. J. Geophys. Res. 1995, 100:11719-11728.
    • (1995) J. Geophys. Res. , vol.100 , pp. 11719-11728
    • Weinstein, S.A.1
  • 81
    • 2542437758 scopus 로고    scopus 로고
    • Tharsis as a consequence of Mars' dichotomy and layered mantle
    • Wenzel M.J., Manga M., Jellinek A.M. Tharsis as a consequence of Mars' dichotomy and layered mantle. Geophys. Res. Lett. 2004, 31:L04702.
    • (2004) Geophys. Res. Lett. , vol.31
    • Wenzel, M.J.1    Manga, M.2    Jellinek, A.M.3
  • 82
    • 63749090256 scopus 로고    scopus 로고
    • The global martian volcanic evolutionary history
    • Werner S.C. The global martian volcanic evolutionary history. Icarus 2009, 201:44-68.
    • (2009) Icarus , vol.201 , pp. 44-68
    • Werner, S.C.1
  • 83
    • 0041841762 scopus 로고
    • An alternative model for the formation of the asteroids
    • Wetherill G.W. An alternative model for the formation of the asteroids. Icarus 1992, 100:307-325.
    • (1992) Icarus , vol.100 , pp. 307-325
    • Wetherill, G.W.1
  • 84
    • 0001189412 scopus 로고
    • The martian dichotomy may be due to a giant impact
    • Wilhelms D.E., Squyres S.W. The martian dichotomy may be due to a giant impact. Nature 1984, 309:138-140.
    • (1984) Nature , vol.309 , pp. 138-140
    • Wilhelms, D.E.1    Squyres, S.W.2
  • 86
    • 62549131294 scopus 로고    scopus 로고
    • Migration of Tharsis volcanism on Mars caused by differential rotation of the lithosphere
    • Zhong S. Migration of Tharsis volcanism on Mars caused by differential rotation of the lithosphere. Nat. Geosci. 2009, 2:19-23.
    • (2009) Nat. Geosci. , vol.2 , pp. 19-23
    • Zhong, S.1
  • 87
    • 0034930921 scopus 로고    scopus 로고
    • Degree-1 mantle convection and the crustal dichotomy on Mars
    • Zhong S., Zuber M.T. Degree-1 mantle convection and the crustal dichotomy on Mars. Earth Planet. Sci. Lett. 2001, 189:75-84.
    • (2001) Earth Planet. Sci. Lett. , vol.189 , pp. 75-84
    • Zhong, S.1    Zuber, M.T.2


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.