M. Davidson et al., Orogenic fluids and secondary magnetizations: testing the relationship in the South Wales Coalfield foreland basin, J GEOCHEM E, 69, 2000, pp. 581-584
Carbonates that rim the South Wales Coalfield contain a pervasive Irate Pal
eozoic CRM residing in magnetite. The CRM in the eastern part of the basin
was acquired after deformation, and geochemical results are consistent with
a connection between remagnetization and orogenic-type fluids. In the west
ern part of the basin, the CRM is synfolding but the geochemical results do
not support a connection with orogenic fluids. (C) 2000 Elsevier Science B
.V. All rights reserved.