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• W12061488 abstract "Abstract A variety of geophysical, petrological and geochemical models for the earth are reviewed. Most deal with either the initial or present states of the earth and do not attempt a comprehensive theory. Convection models and thermal history models assume an initial hot, partly molten earth state with the exception of some two-layer convection models for a cool earth, constructed but rejected by McKenzie and Weiss. Petrological and geochemical models almost all emphasize mantle heterogeneity but are divided into varieties advocating either early major continental growth or steady (perhaps episodic) continental growth. Isotopic constraints have been interpreted in widely differing ways, but the preferred view is that Sr, Pb and Nd isotopes now all indicate progressive growth of the continents with a maximum growth rate in the late Archaean. Recycling has been postulated on chemical and isotopic abundance grounds, but does not appear to be important until the Phanerozoic. These ideas, taken together with a philosophy which equates high heat flow with high rates of continental growth, leads to the author's model of a hot-spot non-plate-tectonic model Archaean, in which interaction of hot-spots (plumes) with primitive oceanic or mini-continental crust can lead to either the granite—greenstone or ancient gneiss type of Archaean crustal complex." @default.
• W12061488 created "2016-06-24" @default.
• W12061488 creator A5086319178 @default.
• W12061488 date "1981-01-01" @default.
• W12061488 modified "2023-09-27" @default.
• W12061488 title "Chapter 18 Earth Tectonics and Thermal History: Review And a Hot-Spot Model for the Archaean" @default.
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• W12061488 doi "https://doi.org/10.1016/s0166-2635(08)70023-9" @default.
• W12061488 hasPublicationYear "1981" @default.
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