Use of micro-XRF chemical analysis for mapping volcanogenic massive sulfide related hydrothermal alteration: Application to the subaqueous felsic dome-flow complex of the Cap d'Ours section, Glenwood rhyolite, Rouyn-Noranda, Québec, Canada

A new analytical method using micro-X-ray fluorescence (XRF) is presented for the in situ analysis of major elements in rock samples. This approach has allowed for a separate study of hydrothermal alteration of matrix versus fragments in volcaniclastic material (i.e. flow breccia). This is particula...

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Veröffentlicht in:	Journal of geochemical exploration 2011-02, Vol.108 (2), p.131-142
Hauptverfasser:	Genna, Dominique, Gaboury, Damien, Moore, Lyndsay, Mueller, Wulf U.
Format:	Artikel
Sprache:	eng
Schlagworte:	Abitibi belt Dome-flow complex Hydrothermal alteration mapping Micro-XRF chemical analysis New-Senator caldera Volcanogenic massive sulfide exploration
Online-Zugang:	Volltext
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