Fig. 5From: Structural, geochemical, and mineralogical investigation of active hydrothermal fluid discharges at Strýtan hydrothermal chimney, Akureyri Bay, Eyjafjörður region, IcelandResults of XRD analysis of sample IS_Strýtan_01 show that the hydrothermal cones are predominantly made up of a trioctahedral phyllosilicate, presumably saponite. Aragonite and hisingerite may also be presentBack to article page