Skip to main content
Article thumbnail
Location of Repository

Cenozoic exhumation of the southern British Isles

By Richard R. Hillis, Simon P. Holford, Paul F. Green, A.G. Dore, Robert Gatliff, Martyn Stoker, Ken Thomson, Jonathan P. Turner, John R. Underhill and Gareth Williams

Abstract

Rocks that crop out across southern Britain were exhumed from depths of as much as 2.5 km during Cenozoic time. This has been widely attributed to Paleocene regional uplift resulting from igneous underplating related to the Iceland mantle plume. Our compilation of paleothermal and compaction data reveals spatial and temporal patterns of exhumation showing little correspondence with the postulated influence of underplating, instead being dominated by kilometer-scale variations across Cenozoic compressional structures, which in several basins are demonstrably of Neogene age. We propose that crustal compression, due to plate boundary forces transmitted into the plate interior, was the major cause of Cenozoic uplift in southern Britain, witnessing a high strength crust in western Europe

Topics: Earth Sciences
Publisher: Geological Society of America
Year: 2008
DOI identifier: 10.1130/G24699A.1
OAI identifier: oai:nora.nerc.ac.uk:6727
Download PDF:
Sorry, we are unable to provide the full text but you may find it at the following location(s):
  • http://geology.geoscienceworld... (external link)
  • https://doi.org/10.1130/G24699... (external link)
  • https://doi.org/10.1130/G24699... (external link)
  • http://nora.nerc.ac.uk/id/epri... (external link)
  • Suggested articles


    To submit an update or takedown request for this paper, please submit an Update/Correction/Removal Request.