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- W2063330441 abstract "Abstract Brittle fault rocks, usually in the form of minor pseudotachylyte veins have been reported from most high-grade metamorphic Archaean and Proterozoic terrains. In analyses of local crustal evolution such brittle structures are often ignored; brittle faults commonly reflect the very last phases of local deformation during final uplift of the basement to shallow crustal levels, and as such they are thought to be of minor or no importance in large-scale Archaean and Proterozoic tectonics. New data from Archaean and Proterozoic high grade terrains in Australia and Antarctica indicate that minor fault veins may in some cases represent significant early low-grade brittle events which have been overprinted and largely erased by subsequent phases of ductile deformation. This paper describes such a brittle event in the Vestfold Hills, East Antarctica, which may represent an important phase of mid-Proterozoic uplift and crustal extension." @default.
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- W2063330441 date "1990-04-01" @default.
- W2063330441 modified "2023-09-27" @default.
- W2063330441 title "Ductile reactivation of Proterozoic brittle fault rocks; an example from the Vestfold Hills, East Antarctica" @default.
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