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

Volumn 150, Issue 1, 2005, Pages 102-118

  Kenis, I ^a   Muchez, Ph ^a   Verhaert, G ^a   Boyce, A ^b   Sintubin, M ^a  

^a UNIVERSITY OF LEUVEN   (Belgium)

^b SCOTTISH UNIVERSITIES ENVIRONMENTAL RESEARCH CENTRE   (United Kingdom)

Author keywords

[No Author keywords available]

Indexed keywords

DEVONIAN; HERCYNIAN OROGENY; HYDROCHEMISTRY; HYDROTHERMAL FLUID; SLATE;

BELGIUM; BENELUX; EASTERN HEMISPHERE; EURASIA; EUROPE; WESTERN EUROPE; WORLD;

EID: 27244451140     PISSN: 00107999     EISSN: None     Source Type: Journal    
DOI: 10.1007/s00410-005-0008-9     Document Type: Article

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