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- W2003148785 abstract "The Caprauna-Armetta Unit (CAU) is a Briançonnais cover nappe emplaced on the external margin of the Ligurian Briançonnais Zone. A structural analysis of the nappe indicates that there are four superposed deformations (D1-D4). D1 produced large recumbent isoclinal folds associated with a strong axial-plane cleavage and a SW-trending lineation. These folds can be related to a SW-directed overthrust shear. D2 produced open to moderately tight folds with subvertical axial planes, overturned towards the northeast. D3 and D4 are represented by large wavelength open folds affecting only the large-scale setting of the nappe. A finite strain map of the nappe has been compiled using data from an oolitic limestone layer. The measured strains appears to be essentially the product of the D1 phase. The measured ellipsoids are generally triaxial. The trend of the finite strain X axes is towards the southwest. Prolate ellipsoids with very high Rxz ratios occur on the inverted limbs and sometimes near the hinge zones of the anticlinal F1 folds. Oblate ellipsoids are prevalent on the normal limbs. This pattern of finite strain resulted from deformation in a ductile shear zone generated within the tectonic units trailed at the base of the huge Helminthoid Flysch Nappe during its motion towards the foreland." @default.
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- W2003148785 date "1988-01-01" @default.
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- W2003148785 title "Structural evolution of a briançonnais cover nappe, the caprauna-armetta unit (ligurian alps, Italy)" @default.
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- W2003148785 doi "https://doi.org/10.1016/0191-8141(88)90028-4" @default.
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