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- W55542969 abstract "Abstract Consideration of heat flow parameters and possible lithospheric transformation and deformation during the Archaean enables constraints to be placed on the geotectonic framework of the early earth. They imply a transformation from primary magmagenesis at random centres, which reflect small-scale convective jets and impact-induced thermal anomalies, to linear ridge systems. Patterns of lithosphere consumption would change in concert with this transformation. The difficulty of eclogite formation, due to steep early geothermal gradients, implies the dominance of shallow-dipping zones of lithosphere consumption. This carries the consequence of secondary magmatism and formation of protocontinental material over broad areas of the early crust. The inter-relation between shallow-dipping imbrication of supracrustals and protosialic material, and calc-alkaline magmatism at the sites of lithosphere consumption helps explain many general features of high-grade Archaean terrains. Hypothetical buckling structures associated with horizontal deformation of sial-capped slabs of thin lithosphere help explain features of low grade terrains. Secular decline in overall heat flow implies, at some point in Precambrian time, the sudden appearance of eclogite-capped, descending lithosphere, steep-dipping subduction with narrow volcanic arcs and decreasing amplitude/wavelength ratios of lithospheric deformation." @default.
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- W55542969 date "1978-01-01" @default.
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- W55542969 title "Basic Factors in Archaean Geotectontcs" @default.
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- W55542969 doi "https://doi.org/10.1016/s0166-2635(08)70089-6" @default.
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