Fig. 6From: The characterisation of an exhumed high-temperature paleo-geothermal system on Terre-de-Haut Island (the Les Saintes archipelago, Guadeloupe) in terms of clay minerals and petrophysicsX-ray diffractograms performed on whole rock. Comparison of fresh (above) and altered facies (below). Pl plagioclase, Opx orthopyroxene, Qz quartz, Crs cristobalite, K-phy K-phyllosilicatesBack to article page