Abstract
An oceanographic survey by H.M.S. Hecla of the 1974 active submarine volcano (12°18′N and 61°38′W) revealed a crater at 190 m below sea level and bottom-sampling yielded fresh olivine basalt pyroclastics with phenocrysts of olivine, plagioclase and clinopyroxene. Megacrysts of amphilbole, up to 16 modal percent, are subsilicic and nepheline-normative ferroan pargasites. The mineral assemblage Ol+Cpx+Pl+Amph appears to have been in equilibrium in the Kick’em-Jenny melt prior to eruption, although published experimental studies on hydrous (H2O-saturated) or anhydrous alkali basaltic compositions have not yielded this mineral assemblage at any pressure. Interpolation between the experimentally determined phase relationships for dry and water-saturated alkali basaltic liquids indicates, however, that in an isobaric section at 5 kb the observed assemblage can exist in the water-undersaturated region. The Kick’em-Jenny olivine basalts belong to a suite of variably undersaturated basaltic rocks including alkali picrites and basanites, common in Grenada and the southern Grenadines, but although the available evidence indicates the importance of the presence of water in the genesis of these melts, their origin seems most likely to be associated with partial melting of upper mantle material rather than melting of amphibolite in an underthrust lithospheric slab.
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Sigurdsson, H., Shepherd, J.B. Amphibole-bearing basalts from the submarine volcano Kick’em-Jenny in the lesser antilles Island arc. Bull Volcanol 38, 891–910 (1974). https://doi.org/10.1007/BF02597097
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DOI: https://doi.org/10.1007/BF02597097