Welsh Borderland Fault System

The Welsh Borderland Fault System is a zone of faulting and associated folding which runs northeastwards through Wales from Pembrokeshire through Carmarthenshire and Powys into Shropshire in England. It comprises the Tywi Lineament, Pontesford Lineament and Church Stretton Fault Zone.[1] The southern margin of the fault system is defined by the Church Stretton Fault and Dulas Valley Fault, amongst others whilst its northern margin is defined by the Garth-Llanwrtyd Fault Belt in Carmarthenshire. The Church Stretton Fault component of the system is deemed to form the terrane boundary between the Cymru Terrane to its northwest and the Wrekin Terrane to its southeast.[2]

The system was active during the Caledonian Orogeny and was reactivated during the later Variscan Orogeny. [3]

References

  1. ↑ Brenchley, P.J. & Rawson, P.F. (eds) 2006 The Geology of England and Wales. The Geological Society, London (p80)
  2. ↑ Brenchley, P.J. & Rawson, P.F. (eds) 2006 The Geology of England and Wales. The Geological Society, London (pp14-15)
  3. ↑ Geology of the Llandovery District - a brief explanation of the geological maps sheet 212 ‘Llandovery’
This article is issued from Wikipedia - version of the Monday, September 09, 2013. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.