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- W3186346723 abstract "Palaeozoic rocks in the Variscan domain of SW Dyfed, Wales, were deformed under anchimetamorphic conditions during the late Carboniferous. Within the Pembrokeshire Coalfield a 1 km wide zone of conjugate folds and thrusts, external to the northern limit of slaty cleavage, is used to define the Variscan orogenic front. South of the front there is a progressive increase in the average amplitude of macrofolds across three further structural zones. Folding about a WNW axial trend was single phase except within a few narrow belts of refolded folds. Wrench and normal faults which developed during and after folding resulted in the axial elongation and clockwise rotation of the region. Structures in the paratectonic Caledonides controlled the locations of four WSW trending Disturbance Belts of Variscan age to the north of the front. In the Druidston Haven-Horst, the westernmost of these Disturbances, Caledonian folds and cleavage were refolded approximately coaxially during the Variscan. The Variscan fold belt is cut by several, laterally impersistent, major strike faults which can not be regarded as separating allochthonous blocks. (32 refs.)" @default.
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- W3186346723 date "1981-03-01" @default.
- W3186346723 modified "2023-09-27" @default.
- W3186346723 title "Variscan structures in southwest Wales" @default.
- W3186346723 hasPublicationYear "1981" @default.
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