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Hydrothermal Alteration of Basaltic Rocks at Eruptive Vents on Mount Cameroon Volcano, West Africa

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Figure

Figure 1. (a) Sketch map of the Cameroon Volcanic Line (CVL) showing the location of Mount Cameroon along the (after NE-SW-trending volcanic chain
Figure 2. Characteristic hydrothermal alteration features of the 1999 eruptive vents. (a) es)
Figure 3. Representative photomicrographs of altered basaltic rocks from the Mount tion
Figure 4. Representative XRD patterns of altered basaltic rocks from the 1999 vents, aug = augite, mag = magnetite, pyx = pyroxene, jar = jarosite
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