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ConMan

By Scott D. King1, Arthur Raefsky, Brad Hager2

1. Virgina Tech 2. Massachusetts Institute of Technology

Citations Non-affiliated (90) | Affiliated (0)

Non-affiliated authors

  • King, S., Raefsky, A., Hager, B. H., (2020), "ConMan version 3.0.0", Zenodo: (DOI: 10.5281/zenodo.3633152). Cited by:

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  • Lim, C., Lee, C., (2015), "Effects of temporal plume-slab interaction on the partial melting of the subducted oceanic crust", Journal of Asian Earth Sciences, 113: pg: 857--865, (DOI: 10.1016/j.jseaes.2015.09.016). Cited by:

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  • Kim, Y. H., Lee, C., Kim, S-S, (2015), "Tectonics and volcanism in East Asia: Insights from geophysical observations", Journal of Asian Earth Sciences, 113: pg: 842--856, (DOI: 10.1016/j.jseaes.2015.07.032). Cited by:

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  • Lee, C., Lim, C., (2014), "Short-term and localized plume-slab interaction explains the genesis of Abukuma adakite in Northeastern Japan", Earth and Planetary Science Letters, 396: pg: 116--124, (DOI: 10.1016/j.epsl.2014.04.009). Cited by:

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  • Kim, Y-M, Lee, C., (2014), "Effect of time-evolving age and convergence rate of the subducting plate on the Cenozoic adakites and boninites", Journal of Asian Earth Sciences, 95: pg: 300--312, (DOI: 10.1016/j.jseaes.2014.06.029). Cited by:

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  • Elkins-Tanton, L. T., (2012), "Magma Oceans in the Inner Solar System", Annual Review of Earth and Planetary Sciences, 40, 1: pg: 113--139, (DOI: 10.1146/annurev-earth-042711-105503). Cited by:

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  • Lee, C., King, S. D., (2011), "Dynamic buckling of subducting slabs reconciles geological and geophysical observations", Earth and Planetary Science Letters, 312, 3-4: pg: 360--370, (DOI: 10.1016/j.epsl.2011.10.033). Cited by:

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  • Han, L., Showman, A. P., (2011), "Coupled convection and tidal dissipation in Europa's ice shell using non-Newtonian grain-size-sensitive (GSS) creep rheology", Icarus, 212, 1: pg: 262--267, (DOI: 10.1016/j.icarus.2010.11.034). Cited by:

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  • Lee, C., King, S. D., (2010), "Why are high-Mg# andesites widespread in the western Aleutians? A numerical model approach", Geology, 38, 7: pg: 583--586, (DOI: 10.1130/G30714.1). Cited by:

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  • King, S. D., Lee, C., Keken, P. E., Leng, W., Zhong, S., Tan, E., Tosi, N., Kameyama, M. C., (2010), "A community benchmark for 2-D Cartesian compressible convection in the Earth's mantle", Geophysical Journal International, 180, 1: pg: 73--87, (DOI: 10.1111/j.1365-246X.2009.04413.x). Cited by:

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  • Han, L., Showman, A. P., (2010), "Coupled convection and tidal dissipation in Europa's ice shell", Icarus, 207, 2: pg: 834--844, (DOI: 10.1016/j.icarus.2009.12.028). Cited by:

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  • Conrad, C. P., Wu, B., Smith, E. I., Bianco, T. A., Tibbetts, A., (2010), "Shear-driven upwelling induced by lateral viscosity variations and asthenospheric shear: A mechanism for intraplate volcanism", Physics of the Earth and Planetary Interiors, 178, 3-4: pg: 162--175, (DOI: 10.1016/j.pepi.2009.10.001). Cited by:

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  • Watters, W. A., Zuber, M. T., Hager, B. H., (2009), "Thermal perturbations caused by large impacts and consequences for mantle convection", Journal of Geophysical Research, 114, E2: pg: E02001, (DOI: 10.1029/2007JE002964). Cited by:

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  • Lee, C., King, S. D., (2009), "Effect of mantle compressibility on the thermal and flow structures of the subduction zones", Geochemistry, Geophysics, Geosystems, 10, 1: pg: Q01006, (DOI: 10.1029/2008GC002151). Cited by:

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  • King, S. D., (2009), "On topography and geoid from 2-D stagnant lid convection calculations", Geochemistry, Geophysics, Geosystems, 10, 3: pg: Q03002, (DOI: 10.1029/2008GC002250). Cited by:

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  • Hebert, L. B., Antoshechkina, P., Asimow, P., Gurnis, M., (2009), "Emergence of a low-viscosity channel in subduction zones through the coupling of mantle flow and thermodynamics", Earth and Planetary Science Letters, 278, 3-4: pg: 243--256, (DOI: 10.1016/j.epsl.2008.12.013). Cited by:

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  • Farnetani, C. G., Hofmann, A. W., (2009), "Dynamics and internal structure of a lower mantle plume conduit", Earth and Planetary Science Letters, 282, 1-4: pg: 314--322, (DOI: 10.1016/j.epsl.2009.03.035). Cited by:

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  • Keken, P. E., Currie, C., King, S. D., Behn, M. D., Cagnioncle, A., He, J., Katz, R. F., Lin, S-C, Parmentier, E. M., Spiegelman, M., Wang, K., (2008), "A community benchmark for subduction zone modeling", Physics of the Earth and Planetary Interiors, 171, 1-4: pg: 187--197, (DOI: 10.1016/j.pepi.2008.04.015). Cited by:

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  • King, S. D., (2008), "ConMan v2.0.0 [software]", Computational Infrastructure for Geodynamics: . Cited by:

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  • Han, L., Showman, A. P., (2008), "Implications of shear heating and fracture zones for ridge formation on Europa", Geophysical Research Letters, 35, 3: pg: L03202, (DOI: 10.1029/2007GL031957). Cited by:

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  • Redmond, H. L., King, S. D., (2007), "Does mantle convection currently exist on Mercury?", Physics of the Earth and Planetary Interiors, 164, 3-4: pg: 221--231, (DOI: 10.1016/j.pepi.2007.07.004). Cited by:

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  • Naliboff, J. B., Kellogg, L. H., (2007), "Can large increases in viscosity and thermal conductivity preserve large-scale heterogeneity in the mantle?", Physics of the Earth and Planetary Interiors, 161, 1-2: pg: 86--102, (DOI: 10.1016/j.pepi.2007.01.009). Cited by:

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  • Long, M. D., Hager, B. H., Hoop, M. V., Hilst, R. D., (2007), "Two-dimensional modelling of subduction zone anisotropy with application to southwestern Japan", Geophysical Journal International, 170, 2: pg: 839--856, (DOI: 10.1111/j.1365-246X.2007.03464.x). Cited by:

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  • Elkins-Tanton, L. T., (2007), "Continental magmatism, volatile recycling, and a heterogeneous mantle caused by lithospheric gravitational instabilities", Journal of Geophysical Research, 112, B3: pg: B03405, (DOI: 10.1029/2005JB004072). Cited by:

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  • Davies, D. R., Davies, J. H., Hassan, O., Morgan, K., Nithiarasu, P., (2007), "Investigations into the applicability of adaptive finite element methods to two-dimensional infinite Prandtl number thermal and thermochemical convection", Geochemistry, Geophysics, Geosystems, 8, 5: pg: Q05010, (DOI: 10.1029/2006GC001470). Cited by:

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  • Coltice, N., Phillips, B. R., Bertrand, H., Ricard, Y., Rey, P., (2007), "Global warming of the mantle at the origin of flood basalts over supercontinents", Geology, 35, 5: pg: 391, (DOI: 10.1130/G23240A.1). Cited by:

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  • Naliboff, J. B., Kellogg, L. H., (2006), "Dynamic effects of a step-wise increase in thermal conductivity and viscosity in the lowermost mantle", Geophysical Research Letters, 33, 12: pg: L12S09, (DOI: 10.1029/2006GL025717). Cited by:

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  • Tan, E., (2005), "Metastable superplumes and mantle compressibility", Geophysical Research Letters, 32, 20: pg: L20307, (DOI: 10.1029/2005GL024190). Cited by:

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  • Showman, A. P., Han, L., (2005), "Effects of plasticity on convection in an ice shell: Implications for Europa", Icarus, 177, 2: pg: 425--437, (DOI: 10.1016/j.icarus.2005.02.020). Cited by:

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  • Mitri, G., Showman, A. P., (2005), "Convective-conductive transitions and sensitivity of a convecting ice shell to perturbations in heat flux and tidal-heating rate: Implications for Europa", Icarus, 177, 2: pg: 447--460, (DOI: 10.1016/j.icarus.2005.03.019). Cited by:

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  • Koglin Jr., D. E., Ghias, S. R., King, S. D., Jarvis, G. T., Lowman, J. P., (2005), "Mantle convection with reversing mobile plates: A benchmark study", Geochemistry, Geophysics, Geosystems, 6, 9: pg: Q09003, (DOI: 10.1029/2005GC000924). Cited by:

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  • Coltice, N., (2005), "The role of convective mixing in degassing the Earth's mantle", Earth and Planetary Science Letters, 234, 1-2: pg: 15--25, (DOI: 10.1016/j.epsl.2005.02.041). Cited by:

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  • Showman, A. P., (2004), "Numerical simulations of convection in Europa's ice shell: Implications for surface features", Journal of Geophysical Research, 109, E1: pg: E01010, (DOI: 10.1029/2003JE002103). Cited by:

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  • Elkins-Tanton, L. T., Hager, B. H., Grove, T. L., (2004), "Magmatic effects of the lunar late heavy bombardment", Earth and Planetary Science Letters, 222, 1: pg: 17--27, (DOI: 10.1016/j.epsl.2004.02.017). Cited by:

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  • Tackley, P. J., King, S. D., (2003), "Testing the tracer ratio method for modeling active compositional fields in mantle convection simulations", Geochemistry, Geophysics, Geosystems, 4, 4: pg: 8302, (DOI: 10.1029/2001GC000214). Cited by:

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  • Samuel, H., Farnetani, C. G., (2003), "Thermochemical convection and helium concentrations in mantle plumes", Earth and Planetary Science Letters, 207, 1-4: pg: 39--56, (DOI: 10.1016/S0012-821X(02)01125-1). Cited by:

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  • Elkins Tanton, L. T., Van Orman, J. A., Hager, B. H., Grove, T. L., (2002), "Re-examination of the lunar magma ocean cumulate overturn hypothesis: melting or mixing is required", Earth and Planetary Science Letters, 196, 3-4: pg: 239--249, (DOI: 10.1016/S0012-821X(01)00613-6). Cited by:

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  • Hunt, D. L., Kellogg, L. H., (2001), "Quantifying mixing and age variations of heterogeneities in models of mantle convection: Role of depth-dependent viscosity", Journal of Geophysical Research: Solid Earth, 106, B4: pg: 6747--6759, (DOI: 10.1029/2000JB900261). Cited by:

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  • Conrad, C. P., Hager, B. H., (2001), "Mantle convection with strong subduction zones", Geophysical Journal International, 144, 2: pg: 271--288, (DOI: 10.1046/j.1365-246x.2001.00321.x). Cited by:

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  • Tanton, L. T. E., Hager, B. H., (2000), "Melt intrusion as a trigger for lithospheric foundering and the eruption of the Siberian flood basalts", Geophysical Research Letters, 27, 23: pg: 3937--3940, (DOI: 10.1029/2000GL011751). Cited by:

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  • Conrad, C. P., (2000), "Convective instability of thickening mantle lithosphere", Geophysical Journal International, 143, 1: pg: 52--70, (DOI: 10.1046/j.1365-246x.2000.00214.x). Cited by:

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  • Sidorin, I., Gurnis, M., Helmberger, D. V., (1999), "Dynamics of a phase change at the base of the mantle consistent with seismological observations", Journal of Geophysical Research: Solid Earth, 104, B7: pg: 15005--15023, (DOI: 10.1029/1999JB900065). Cited by:

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  • Shapiro, S. S., Hager, B. H., Jordan, T. H., R.D. van der Hilst and W.F. McDonough (1999), "Developments in Geotectonics", Stability and dynamics of the continental tectosphere, Elsevier, 48, 1-4: pg: 115--133, 0419-0254, (DOI: 10.1016/S0419-0254(99)80008-1). Cited by:

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  • Rowland, A., Davies, J. H., (1999), "Buoyancy rather than rheology controls the thickness of the overriding mechanical lithosphere at subduction zones", Geophysical Research Letters, 26, 19: pg: 3037--3040, (DOI: 10.1029/1999GL005347). Cited by:

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  • Han, L., Gurnis, M., (1999), "How valid are dynamic models of subduction and convection when plate motions are prescribed?", Physics of the Earth and Planetary Interiors, 110, 3-4: pg: 235--246, (DOI: 10.1016/S0031-9201(98)00156-3). Cited by:

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  • Conrad, C. P., Molnar, P., (1999), "Convective instability of a boundary layer with temperature-and strain-rate-dependent viscosity in terms of 'available buoyancy'", Geophysical Journal International, 139, 1: pg: 51--68, (DOI: 10.1046/j.1365-246X.1999.00896.x). Cited by:

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  • Coltice, N., Ricard, Y., (1999), "Geochemical observations and one layer mantle convection", Earth and Planetary Science Letters, 174, 1-2: pg: 125--137, (DOI: 10.1016/S0012-821X(99)00258-7). Cited by:

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  • Becker, T. W., Faccenna, C., O'Connell, R. J., Giardini, D., (1999), "The development of slabs in the upper mantle: Insights from numerical and laboratory experiments", Journal of Geophysical Research: Solid Earth, 104, B7: pg: 15207--15226, (DOI: 10.1029/1999JB900140). Cited by:

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  • Montague, N. L., Kellogg, L. H., Manga, M., (1998), "High Rayleigh number thermo-chemical models of a dense boundary layer in D``", Geophysical Research Letters, 25, 13: pg: 2345--2348, (DOI: 10.1029/98GL51872). Cited by:

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  • Lenardic, A., (1998), "On the partitioning of mantle heat loss below oceans and continents over time and its relationship to the Archaean paradox: Mantle heat partitioning and the Archaean paradox", Geophysical Journal International, 134, 3: pg: 706--720, (DOI: 10.1046/j.1365-246x.1998.00604.x). Cited by:

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  • King, S. D., Anderson, D. L., (1998), "Edge-driven convection", Earth and Planetary Science Letters, 160, 3-4: pg: 289--296, (DOI: 10.1016/S0012-821X(98)00089-2). Cited by:

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  • Ita, J., King, S. D., (1998), "The influence of thermodynamic formulation on simulations of subduction zone geometry and history", Geophysical Research Letters, 25, 9: pg: 1463--1466, (DOI: 10.1029/98GL51033). Cited by:

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  • Chen, J., King, S. D., (1998), "The influence of temperature and depth dependent viscosity on geoid and topography profiles from models of mantle convection", Physics of the Earth and Planetary Interiors, 106, 1-2: pg: 75--92, (DOI: 10.1016/S0031-9201(97)00110-6). Cited by:

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  • Keken, P. E., King, S. D., Schmeling, H., Christensen, U. R., Neumeister, D., Doin, M-P, (1997), "A comparison of methods for the modeling of thermochemical convection", Journal of Geophysical Research: Solid Earth, 102, B10: pg: 22477--22495, (DOI: 10.1029/97JB01353). Cited by:

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  • Moresi, L-N, Lenardic, A., (1997), "Three-dimensional numerical simulations of crustal deformation and subcontinental mantle convection", Earth and Planetary Science Letters, 150, 3-4: pg: 233--243, (DOI: 10.1016/S0012-821X(97)00093-9). Cited by:

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  • Kellogg, L. H., King, S. D., (1997), "The effect of temperature dependent viscosity on the structure of new plumes in the mantle: Results of a finite element model in a spherical, axisymmetric shell", Earth and Planetary Science Letters, 148, 1-2: pg: 13--26, (DOI: 10.1016/S0012-821X(97)00025-3). Cited by:

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  • Kellogg, L. H., (1997), "Growing the Earth's D`` layer: Effect of density variations at the core-mantle boundary", Geophysical Research Letters, 24, 22: pg: 2749--2752, (DOI: 10.1029/97GL02952). Cited by:

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  • Zhong, S., Gurnis, M., Moresi, L., (1996), "Free-surface formulation of mantle convection-I. Basic theory and application to plumes", Geophysical Journal International, 127, 3: pg: 708--718, (DOI: 10.1111/j.1365-246X.1996.tb04049.x). Cited by:

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  • Moresi, L., Zhong, S., Gurnis, M., (1996), "The accuracy of finite element solutions of Stokes's flow with strongly varying viscosity", Physics of the Earth and Planetary Interiors, 97, 1-4: pg: 83--94, (DOI: 10.1016/0031-9201(96)03163-9). Cited by:

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  • Lenardic, A., Kaula, W. M., (1996), "Near-surface thermal/chemical boundary layer convection at infinite Prandtl number: two-dimensional numerical experiments", Geophysical Journal International, 126, 3: pg: 689--711, (DOI: 10.1111/j.1365-246X.1996.tb04698.x). Cited by:

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  • Larson, R. L., Kincaid, C., (1996), "Onset of mid-Cretaceous volcanism by elevation of the 670 km thermal boundary layer", Geology, 24, 6: pg: 551, (DOI: 10.1130/0091-7613(1996)024<0551:OOMCVB>2.3.CO;2). Cited by:

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  • Zhong, S., Gurnis, M., (1995), "Towards a realistic simulation of plate margins in mantle convection", Geophysical Research Letters, 22, 8: pg: 981--984, (DOI: 10.1029/95GL00782). Cited by:

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  • Puster, P., Jordan, T. H., Hager, B. H., (1995), "Characterization of mantle convection experiments using two-point correlation functions", Journal of Geophysical Research: Solid Earth, 100, B4: pg: 6351--6365, (DOI: 10.1029/94JB03268). Cited by:

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  • Puster, P., Hager, B. H., Jordan, T. H., (1995), "Mantle convection experiments with evolving plates", Geophysical Research Letters, 22, 16: pg: 2223--2226, (DOI: 10.1029/95GL01998). Cited by:

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  • Lenardic, A., Kaula, W. M., Bindschadler, D. L., (1995), "Some effects of a dry crustal flow law on numerical simulations of coupled crustal deformation and mantle convection on Venus", Journal of Geophysical Research, 100, E8: pg: 16949, (DOI: 10.1029/95JE01895). Cited by:

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  • Lenardic, A., Kaula, W. M., (1995), "More thoughts on convergent crustal plateau formation and mantle dynamics with regard to Tibet", Journal of Geophysical Research: Solid Earth, 100, B8: pg: 15193--15203, (DOI: 10.1029/95JB01289). Cited by:

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  • Zhong, S., Gurnis, M., (1994), "Role of plates and temperature-dependent viscosity in phase change dynamics", Journal of Geophysical Research, 99, B8: pg: 15903, (DOI: 10.1029/94JB00545). Cited by:

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  • Lenardic, A., Kaula, W. M., (1994), "Tectonic plates, D`` thermal structure, and the nature of mantle plumes", Journal of Geophysical Research, 99, B8: pg: 15697, (DOI: 10.1029/94JB00466). Cited by:

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  • Lenardic, A., Kaula, W. M., (1994), "Self-lubricated mantle convection: Two-dimensional models", Geophysical Research Letters, 21, 16: pg: 1707--1710, (DOI: 10.1029/94GL01464). Cited by:

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  • King, S. D., Hager, B. H., (1994), "Subducted slabs and the geoid: 1. Numerical experiments with temperature-dependent viscosity", Journal of Geophysical Research: Solid Earth, 99, B10: pg: 19843--19852, (DOI: 10.1029/94JB01552). Cited by:

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  • Ita, J., King, S. D., (1994), "Sensitivity of convection with an endothermic phase change to the form of governing equations, initial conditions, boundary conditions, and equation of state", Journal of Geophysical Research, 99, B8: pg: 15919, (DOI: 10.1029/94JB00852). Cited by:

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  • Gurnis, M., Torsvik, T. H., (1994), "Rapid drift of large continents during the late Precambrian and Paleozoic: Paleomagnetic constraints and dynamic models", Geology, 22, 11: pg: 1023, (DOI: 10.1130/0091-7613(1994)022<1023:RDOLCD>2.3.CO;2). Cited by:

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  • Gaherty, J. B., Hager, B. H., (1994), "Compositional vs. thermal buoyancy and the evolution of subducted lithosphere", Geophysical Research Letters, 21, 2: pg: 141--144, (DOI: 10.1029/93GL03466). Cited by:

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  • Farnetani, C. G., Richards, M. A., (1994), "Numerical investigations of the mantle plume initiation model for flood basalt events", Journal of Geophysical Research: Solid Earth, 99, B7: pg: 13813--13833, (DOI: 10.1029/94JB00649). Cited by:

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  • Zhong, S., Gurnis, M., Hulbert, G., (1993), "Accurate determination of surface normal stress in viscous flow from a consistent boundary flux method", Physics of the Earth and Planetary Interiors, 78, 1-2: pg: 1--8, (DOI: 10.1016/0031-9201(93)90078-N). Cited by:

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  • Zhong, S., Gurnis, M., (1993), "Dynamic feedback between a continentlike raft and thermal convection", Journal of Geophysical Research: Solid Earth, 98, B7: pg: 12219--12232, (DOI: 10.1029/93JB00193). Cited by:

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  • Lenardic, A., Kaula, W. M., Bindschadler, D. L., (1993), "A mechanism for crustal recycling on Venus", Journal of Geophysical Research, 98, E10: pg: 18697, (DOI: 10.1029/93JE01799). Cited by:

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  • Lenardic, A., Kaula, W. M., (1993), "A numerical treatment of geodynamic viscous flow problems involving the advection of material interfaces", Journal of Geophysical Research: Solid Earth, 98, B5: pg: 8243--8260, (DOI: 10.1029/92JB02858). Cited by:

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  • Kiefer, W. S., (1993), "Mantle viscosity stratification and flow geometry: Implications for surface motions on Earth and Venus", Geophysical Research Letters, 20, 4: pg: 265--268, (DOI: 10.1029/93GL00129). Cited by:

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  • Kellogg, L. H., King, S. D., (1993), "Effect of mantle plumes on the growth of D`` by reaction between the core and mantle", Geophysical Research Letters, 20, 5: pg: 379--382, (DOI: 10.1029/93GL00045). Cited by:

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  • Zhong, S., Gurnis, M., (1992), "Viscous flow model of a subduction zone with a faulted lithosphere: Long and short wavelength topography, gravity and geoid", Geophysical Research Letters, 19, 18: pg: 1891--1894, (DOI: 10.1029/92GL02142). Cited by:

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  • Squyres, S. W., Jankowski, D. G., Simons, M., Solomon, S. C., Hager, B. H., McGill, G. E., (1992), "Plains tectonism on Venus: The deformation belts of Lavinia Planitia", Journal of Geophysical Research, 97, E8: pg: 13579, (DOI: 10.1029/92JE00481). Cited by:

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  • Davies, J. H., Stevenson, D. J., (1992), "Physical model of source region of subduction zone volcanics", Journal of Geophysical Research: Solid Earth, 97, B2: pg: 2037--2070, (DOI: 10.1029/91JB02571). Cited by:

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  • Lenardic, A., Kaula, W. M., Bindschadler, D. L., (1991), "The tectonic evolution of Western Ishtar Terra, Venus", Geophysical Research Letters, 18, 12: pg: 2209--2212, (DOI: 10.1029/91GL02734). Cited by:

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  • Kellogg, L. H., (1991), "Interaction of plumes with a compositional boundary at 670 km", Geophysical Research Letters, 18, 5: pg: 865--868, (DOI: 10.1029/91GL01066). Cited by:

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  • King, S. D., Raefsky, A., Hager, B. H., (1990), "Conman: vectorizing a finite element code for incompressible two-dimensional convection in the Earth's mantle", Physics of the Earth and Planetary Interiors, 59, 3: pg: 195--207, (DOI: 10.1016/0031-9201(90)90225-M). Cited by:

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  • King, S. D., Hager, B. H., (1990), "The relationship between plate velocity and trench viscosity in Newtonian and power-law subduction calculations", Geophysical Research Letters, 17, 13: pg: 2409--2412, (DOI: 10.1029/GL017i013p02409). Cited by:

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  • Humphreys, E. D., Hager, B. H., (1990), "A kinematic model for the Late Cenozoic development of southern California crust and upper mantle", Journal of Geophysical Research, 95, B12: pg: 19747, (DOI: 10.1029/JB095iB12p19747). Cited by:

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  • Gurnis, M., (1990), "Plate-mantle coupling and continental flooding", Geophysical Research Letters, 17, 5: pg: 623--626, (DOI: 10.1029/GL017i005p00623). Cited by:

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  • Lenardic, A., "A new class of equilibrium geotherms in the deep thermal lithosphere of continents", Earth and Planetary Science Letters, 176, 3-4: pg: 331--338, (DOI: 10.1016/S0012-821X(00)00025-X). Cited by:

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