Université de Neuchâtel

Evolution of synmetamorphic veins and their wallrocks through a Western Alps transect : no evidence for large-scale fluid flow. Stable isotope, major- and trace-element systematics

Henry, C. ; Burkhard, Martin ; Goffé, B.

In: Chemical Geology, 1996, vol. 127, p. 81-109

Quartz-rich synfolial veins and wallrocks from different areas of a Western Alps cross-section are examined in an attempt to constrain the scale and mechanisms of fluid flow through metamorphic terrains. Different portions of this cross-section underwent distinct P-T evolutions as reflected by the mineralogy of veins: (a) in the greenschist external Dauphinois domain, veins are characterized by...

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