Stratified, coherent, low- to medium-amplitude reflections within volcanic edifices have been consistently interpreted as volcaniclastic deposits, and this relationship is observed across a range of geological settings and magma compositions: Mafic systems: In the FaroeShetland Basin, hyaloclastite foresets at the front of lava deltas form medium-amplitude, prograding reflections that downlap onto the underlying substrate 56,57
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