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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:
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:
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:
Gurnis, M., (1990), "Plate-mantle coupling and continental flooding", Geophysical Research Letters, 17, 5: pg: 623--626, (DOI: 10.1029/GL017i005p00623). Cited by:
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:
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:
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:
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:
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:
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:
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:
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:
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:
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:
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:
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:
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:
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:
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:
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:
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:
King, S., Raefsky, A., Hager, B. H., (2020), "ConMan version 3.0.0", Zenodo: (DOI: 10.5281/zenodo.3633152). Cited by:
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:
King, S. D., (2008), "ConMan v2.0.0 [software]", Computational Infrastructure for Geodynamics: . Cited by:
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:
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:
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:
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:
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:
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:
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:
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:
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:
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:
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:
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:
Lenardic, A. and Moresi, L., (2000), "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:
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:
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:
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:
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:
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:
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:
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:
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:
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:
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:
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:
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:
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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