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- W2000661483 abstract "Abstract The structure is described of a 12 km transect across the Central Wales ‘Syncline’ of the Welsh Caledonides. The fold is a complex SE-verging structure with a strike-faulted core, involving only Llandovery Series (Lower Silurian) turbidites at outcrop. This fault-fold lineament is thought to overlie a transpressively reactivated NW-dipping fault, originally a normal fault that laterally confined the Rhuddnant turbidite system to its hangingwall. The Acadian (?early Devonian) folds are commonly clockwise-transected by their associated cleavage. This is attributed to homogeneous sinistral transpression in the cover with a component of heterogeneous strain above the reactivated basement fault. The core and steep limb of the major syncline show high transection angles. This leads to a general model where the strike-slip components in transpression are preferentially partitioned into steep faults or into zones of steep bedding." @default.
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- W2000661483 date "1990-01-01" @default.
- W2000661483 modified "2023-10-18" @default.
- W2000661483 title "Transpressive Acadian deformation across the Central Wales lineament" @default.
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- W2000661483 doi "https://doi.org/10.1016/0191-8141(90)90017-s" @default.
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