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- W2074144977 abstract "Two granite plutons in the Pan-African belt of Hoggar, Algeria, are studied using the anisotropy of magnetic susceptibility technique (AMS) at low-field, together with a study of microstructures. The Tesnou Complex is made of coalescent plutons at the margins of which dextral N-S-oriented shearing imprints solid-state textures. In the granite, microstructures and low magnetic anisotropy magnitudes indicate a magmatic-state weak deformation. Consistent NW-SE-trending sub-horizontal magnetic lineations, making an overall oblique pattern with respect to bordering shear faults, is attributed to low N-S-trending dextral shear strain magnitudes (γ < 1.5) recorded by the magma in its site of emplacement. In the Tioueine pluton, microstructures are also dominantly magmatic except along the western margin and at the contact with an internal unit. Fabrics have homogeneous N-S trends in the central part of the pluton and bend to NNE-SSW trends on the northern and southern edges, thus forming a sigmoidal pattern. The overall fabric pattern is interpreted as for the Tesnou, but with an additional ≈30° clockwise bulk rotation of the pluton during its emplacement. These late-orogenic granites emplaced in bulk tensional sites of the brittle crust, are coeval with the late N-S dextral shear zones that characterize the end of the Pan-African orogeny." @default.
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- W2074144977 date "1997-09-01" @default.
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- W2074144977 title "Oblique magmatic structures of two epizonal granite plutons, Hoggar, Algeria: late-orogenic emplacement in a transcurrent orogen" @default.
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- W2074144977 doi "https://doi.org/10.1016/s0040-1951(97)00123-6" @default.
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