Antun, P. (1954) Sur des paramorphoses de cubes de pyrite et le mode de formation métamorphique de quelques sulfures de l'Ardenne. Annales de la Société géologique de Belgique, 77, B343.

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	Heijlen, Wouter, Muchez, Philippe, Banks, David A. (2001) Origin and evolution of high-salinity, Zn-Pb mineralising fluids in the Variscides of Belgium. Mineralium Deposita, 36 (2) 165-176 doi:10.1007/s001260050296	Journal (article/letter/editorial)
	Zn±Pb mineralising ¯uids in the Variscides of Belgium Received: 26 April 2000 / Accepted: 22 November...deposits in the Verviers Synclinorium (eastern Belgium) and in Cretaceous vein calcites at the Variscan...at the southern margin of the Caledonian Brabant Massif in the Late Palaeozoic. The Na±Ca±K content (Na:...U.Leuven, Celestijnenlaan 200C, 3001 Heverlee, Belgium e-mail: wouter.heijlen@geo.kuleuven.ac.be Fax:...evaporites, such as in the Variscides of southern Belgium, or of Palaeozoic high-salinity ¯uids in western
	*Lecomte, P., Sondag, F. (1980) Regional geochemical reconnaissance in the Belgian Ardennes: Secondary dispersion patterns in stream sediments. Mineralium Deposita, 15 (1) doi:10.1007/bf00202844*	Journal (article/letter/editorial)
	Geochemistry, University of Louvain, Louvain-la-Neuve, Belgium Two geochemical stream sediment surveys were conducted...mineral concentrations, has been little applied in Belgium. The first published reports date from 1971 (Dijkstra... The most important metalliferous deposits in Belgium occur chiefly along the Meuse Valley particularly...occur south and south-west and are essentially pyrite-sphalerite-galena ore bodies. Some copper (chalcopyrite)...studies. P. Lecomte and F. Sondag of the Stavelot Massif. The strike of these formations is north east-south
	*Fuchs, K., von Gehlen, K., Mälzer, H., Murawski, H., Semmel, A. - Eds.* (1983) Plateau Uplift - The Rhenish Shield - A Case History. Springer Berlin Heidelberg. doi:10.1007/978-3-642-69219-2**	Book
	using, as their example, the wellstudied Rhenish Massif. After preparatory discussions within the National...and their causes using, as example, the Rhenish Massif. The aim of this programme was to study questions...no longer define a uniform uplift of the Rhenish Massif. Rather, there exists episodic uplift with several...investigation of the Rheinische Schild. (i.e., the Rhenish Massif east and west of the River Rhine). Seventeen geoscientists...' Contents 1 Plateau Uplift of the Rhenish Massif - Introductory Remarks J.H. Illies and K. Fuchs
	*Rutten, M. G. (1969) The Geology of Western Europe. Elsevier, Amsterdam.*	Book
	2s ee oe cen ere Southern border of the Brabant Massif, . =. write 0a seeps) = 3) or oe, Nappe structure...2 = cae AO a ee eee ae ee ee I a km Caledonian ‘massif’. 2... .y.. -snqe- 9% So Ses =, Se ee ee Fépin...intermediate character of the Armorican Massif ne BMOVernan = 5 2 ss we MASSIF ........... 3%. bot phen Mol...CHAPTER 8. THE MASSIF CENTRAL HOROCTC HOM MEME FESS Se ss 4s 8 ke a es “Massif Central” and “Plateau...avai tallest um A a The: Argentera (Mercantouc)i Massif 2) =a ee creer ys) sence ance ee ree 279 279 279

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Pyrite from Serpont massif, Libramont-Chevigny, Luxembourg, Wallonia, Belgium

Pyrite from
Serpont massif, Libramont-Chevigny, Luxembourg, Wallonia, Belgium