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Recycling of oceanic crust and sediment is a common mechanism to account for the presence of chemical heterogeneities observed in oceanic island basalts (OIBs). Because of the sizeable fractionation of lithium isotopes in low‐temperature environments, lithium serves as a tracer for recycled material in OIB sources. In this study, we analyzed 88 samples of Hawaiian basalt from all volcanic stages and...
Hawaiian Volcanoes, From Source to Surface is the outcome of an AGU Chapman Conference held on the Island of Hawai'i in August 2012. As such, this monograph contains a diversity of research results that highlight the current understanding of how Hawaiian volcanoes work and point out fundamental questions requiring additional exploration. Volume highlights include:
Studies that span a range of depths...
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