Fluid evolution during burial and Variscan deformation in the Lower Devonian rocks of the High-Ardenne slate belt (Belgium): sources and causes of high-salinity and C-O-H-N fluids

Boyce, A. (2005) Fluid evolution during burial and Variscan deformation in the Lower Devonian rocks of the High-Ardenne slate belt (Belgium): sources and causes of high-salinity and C-O-H-N fluids. Contributions to Mineralogy and Petrology, 150(1), pp. 102-118. (doi:10.1007/s00410-005-0008-9)

Full text not currently available from Enlighten.


Item Type:Articles
Status:Published
Refereed:Yes
Glasgow Author(s) Enlighten ID:Boyce, Professor Adrian
Authors: Boyce, A.
College/School:College of Science and Engineering > Scottish Universities Environmental Research Centre
Journal Name:Contributions to Mineralogy and Petrology

University Staff: Request a correction | Enlighten Editors: Update this record