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• W2000698783 abstract "The peridotite-gabbro nappe of the Massif du Sud has been mapped with special attention to its structural characteristics. Its structures are found to be remarkably homogeneous over 6000 km2, making it possible to derive a structural and kinematic model of the oceanic uppermost mantle and lower crust. The truncation at ~8 km beneath the sea floor in the ocean from which the thrust originated was nearly horizontal. Foliations in the overlying mantle were moderately dipping; considering the dominant shear sense, the plastic-flow plane was nearly horizontal when frozen while moving away from the ridge. Plastic strain greatly increases upward in the peridotites, culminating in the transition zone between harzburgites, dunites and wehrlites-gabbros. All the contacts between these lithological units were horizontal but the layering in cumulates was variably inclined. The flow lineations in mantle rocks are oriented N—S with regular regional fluctuations. An E—W trending oceanic ridge is deduced from their orientation." @default.
• W2000698783 created "2016-06-24" @default.
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• W2000698783 date "1980-10-01" @default.
• W2000698783 modified "2023-10-18" @default.
• W2000698783 title "Structures in the new caledonia peridotites-gabbros: Implications for oceanic mantle and crust" @default.
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• W2000698783 doi "https://doi.org/10.1016/0040-1951(80)90128-6" @default.
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