"Boudinage" in the High-Ardenne slate belt (Belgium), reconsidered from the perspective of the "interboudin" veins

"Boudinage" in the High-Ardenne slate belt (Belgium), reconsidered from the perspective of the "interboudin" veins

The origin of the "boudins" and the associated "interboudin" veins in the High-Ardenne slate belt (Belgium) has always been a matter of controversy. The question is whether or not they are the result of the process of boudinage. Based on geometric, microthermometric and geochemic...

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Veröffentlicht in:Journal of geochemical exploration 2000, Vol.69, p.511-516
Hauptverfasser: Sintubin, Manuel, Kenis, Ilse, Schroyen, Kristof, Muchez, Philippe, Burke, E
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container_title Journal of geochemical exploration
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creator Sintubin, Manuel
Kenis, Ilse
Schroyen, Kristof
Muchez, Philippe
Burke, E
description The origin of the "boudins" and the associated "interboudin" veins in the High-Ardenne slate belt (Belgium) has always been a matter of controversy. The question is whether or not they are the result of the process of boudinage. Based on geometric, microthermometric and geochemical data, we suggest a close temporal relationship between slaty-cleavage and vein development, placing the origin of the "boudins" and "interboudin" veins entirely during the Variscan compressional event. Microthermometry of the fluid inclusions in the "interboudin" veins allows constraining P-T conditions, which vary between 255 and 145 MPa at 500 degrees C. (C) 2000 Elsevier Science B.V. All rights reserved.
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title "Boudinage" in the High-Ardenne slate belt (Belgium), reconsidered from the perspective of the "interboudin" veins
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