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- W1995802100 abstract "The late Precambrian Damara Supergroup was deposited in a geosyncline. There is good evidence that the intracratonic branch of this geosyncline began its development with a stage of rifting which produced three widely spaced grabens in sialic crust. During a second stage of subsidence the grabens merged and formed a geosyncline. A third stage produced intense deformation associated with thrusting and nappe transport, high-grade metamorphism, anatexis and large-scale granodioritic to granitic plutonism. A discussion of lifely geodynamic interpretations leads to the conclusion that the development of the intracratonic geosyncline can be best explained by a multiple aulacogen model. The dynamics of the orogeny cannot be readily interpreted with the help of a plate tectonic subduction-collision model. Concepts based on Ramberg's (1972) gravitational instability models are considered applicable. The hypothesis is advanced that grabens, aulacogens and mobile belts may represent diverse responses of the crust to astenoliths of different sizes." @default.
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- W1995802100 date "1977-12-01" @default.
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- W1995802100 title "The intracratonic branch of the Damara Orogen in South West Africa I. Discussion of geodynamic models" @default.
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