Understanding Fluid Flow during Tectonic Reactivation: An Example from the Flamborough Head Chalk Outcrop (UK)

Flamborough Head chalks are located at the extremities of E-W and N-S trending fault systems along the Yorkshire coast (UK). Rock deformation is expressed in Selwicks Bay where a normal fault is exposed along with a high density of calcite veins. The fault mineralization is tested using geochemistry...

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Bibliographic Details
Main Authors: O. Faÿ-Gomord, C. Allanic, M. Verbiest, R. Honlet, F. Champenois, M. Bonifacie, C. Chaduteau, S. Wouters, P. Muchez, E. Lasseur, R. Swennen
Format: Article
Language:English
Published: Wiley 2018-01-01
Series:Geofluids
Online Access:http://dx.doi.org/10.1155/2018/9352143
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