PARAMETERIZED CONVECTION AND THE THERMAL EVOLUTION OF THE EARTH

[1] WERE ARCHEAN CONTINENTAL GEOTHERMAL GRADIENTS MUCH STEEPER THAN THOSE OF TODAY [J]. NATURE, 1978, 272 (5650) : 240 - 241

[2] Cathles L.M., 1975, VISCOSITY EARTHS MAN

[3] WHOLE-MANTLE CONVECTION AND PLATE TECTONICS [J]. GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1977, 49 (02): : 459 - 486

[4] HOLMES A, 1915, GEOL MAG, V62, P60

[5] HOLMES A, 1931, 18 T GEOL SOC GLASG, V18, P559

[6] KELVIN L, 1863, PHILOS MAG, V25, P1

[7] KOHLSTEDT DL, 1976, PHYS CHEM MINER, P35

[8] STEADY AND TRANSIENT THERMAL-CONVECTION IN A FLUID LAYER WITH UNIFORM VOLUMETRIC ENERGY-SOURCES [J]. JOURNAL OF FLUID MECHANICS, 1977, 83 (NOV) : 375 - 395

[9] 650-KM SEISMIC DISCONTINUITY [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1979, 42 (02) : 202 - 208

[10] MCKENZIE D, 1975, GEOPHYS J ROY ASTR S, V42, P131, DOI 10.1111/j.1365-246X.1975.tb05855.x

[1] WERE ARCHEAN CONTINENTAL GEOTHERMAL GRADIENTS MUCH STEEPER THAN THOSE OF TODAY [J]. NATURE, 1978, 272 (5650) : 240 - 241

[2] Cathles L.M., 1975, VISCOSITY EARTHS MAN

[3] WHOLE-MANTLE CONVECTION AND PLATE TECTONICS [J]. GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1977, 49 (02): : 459 - 486

[4] HOLMES A, 1915, GEOL MAG, V62, P60

[5] HOLMES A, 1931, 18 T GEOL SOC GLASG, V18, P559

[6] KELVIN L, 1863, PHILOS MAG, V25, P1

[7] KOHLSTEDT DL, 1976, PHYS CHEM MINER, P35

[8] STEADY AND TRANSIENT THERMAL-CONVECTION IN A FLUID LAYER WITH UNIFORM VOLUMETRIC ENERGY-SOURCES [J]. JOURNAL OF FLUID MECHANICS, 1977, 83 (NOV) : 375 - 395

[9] 650-KM SEISMIC DISCONTINUITY [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1979, 42 (02) : 202 - 208

[10] MCKENZIE D, 1975, GEOPHYS J ROY ASTR S, V42, P131, DOI 10.1111/j.1365-246X.1975.tb05855.x