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- W2023285280 abstract "The evolution of ductile shear zones within the Portoro Limestone of the Tuscan Nappe, Portovenere region, Italy, has been determined using three-dimensional strain analysis. Shear zones, composed of calcite matrix and carbonate veins, are parallel to bedding and alternate with undeformed layers of mixed calcite and dolomite. The shear zones developed under conditions of non-coaxial, rotational deformation as determined from the rotation and shape change of veins within the shear zones and the angular relationship between the shear zone fabric and shear zone boundary. In addition, apparently complex flow that would be recorded by additional components of strain, such as layer-parallel shortening or extension or wrenching did not occur based on the lack of significant veins strike changes and pellet shape changes in sections parallel to the shear plane. Minor, localized volume loss occurred in some shear zones where high and low strains are juxtaposed. The shear zones, therefore, developed under conditions of non-coaxial rotational strain that was heterogeneously distributed along layers parallel to bedding and were locally accompanied by volume loss." @default.
- W2023285280 created "2016-06-24" @default.
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- W2023285280 date "1992-02-01" @default.
- W2023285280 modified "2023-09-23" @default.
- W2023285280 title "Evolution of stacked, ductile shear zones in carbonates from mid-crustal levels: Tuscan Nappe, N. Apennines, Italy" @default.
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- W2023285280 doi "https://doi.org/10.1016/0191-8141(92)90055-2" @default.
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