NO WATER, NO GRANITES - NO OCEANS, NO CONTINENTS

[1] HEAT LOSS FROM EARTH - CONSTRAINT ON ARCHAEAN TECTONICS FROM RELATION BETWEEN GEOTHERMAL GRADIENTS AND RATE OF PLATE PRODUCTION [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1978, 40 (03) : 301 - 315

[2] BICKLE MJ, CONTR MINERAL PETROL

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

[4] CAMPBELL IH, PRECAMBRIAN RES

[5] FINK J, 1980, GEOLOGY, V8, P250, DOI 10.1130/0091-7613(1980)8<250:SFAVOR>2.0.CO

[6] 2

[7] ORIGIN OF SOME MAGMAS IN OCEANIC AND CIRCUM-OCEANIC REGIONS [J]. TECTONOPHYSICS, 1973, 17 (03) : 211 - 222

[8] MERCURY SOIL - PRESENCE OF FE2+ [J]. JOURNAL OF GEOPHYSICAL RESEARCH, 1979, 84 (NB13): : 7664 - 7668

[9] EVOLUTION OF PRECAMBRIAN CRUST FROM STRONTIUM ISOTOPIC EVIDENCE [J]. NATURE, 1975, 254 (5499) : 395 - 398

[10] NICHOLLS IA, 1973, J GEOL, V81, P1665

[1] HEAT LOSS FROM EARTH - CONSTRAINT ON ARCHAEAN TECTONICS FROM RELATION BETWEEN GEOTHERMAL GRADIENTS AND RATE OF PLATE PRODUCTION [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1978, 40 (03) : 301 - 315

[2] BICKLE MJ, CONTR MINERAL PETROL

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

[4] CAMPBELL IH, PRECAMBRIAN RES

[5] FINK J, 1980, GEOLOGY, V8, P250, DOI 10.1130/0091-7613(1980)8<250:SFAVOR>2.0.CO

[6] 2

[7] ORIGIN OF SOME MAGMAS IN OCEANIC AND CIRCUM-OCEANIC REGIONS [J]. TECTONOPHYSICS, 1973, 17 (03) : 211 - 222

[8] MERCURY SOIL - PRESENCE OF FE2+ [J]. JOURNAL OF GEOPHYSICAL RESEARCH, 1979, 84 (NB13): : 7664 - 7668

[9] EVOLUTION OF PRECAMBRIAN CRUST FROM STRONTIUM ISOTOPIC EVIDENCE [J]. NATURE, 1975, 254 (5499) : 395 - 398

[10] NICHOLLS IA, 1973, J GEOL, V81, P1665