Basalts occur everywhere—from divergent and convergent plate boundaries to hot spot volcanic chains and major flood basalt provinces. In this chapter, petrological charac- teristics of Mid-Oceanic Ridge Basalts (MORB) and Hawaiian basalts are discussed. We will explore what such characteristics tell us about their modes of origin.
CITATION STYLE
Sen, G. (2014). Basaltic Magmatism at Mid-Oceanic Ridges and Hawaiian Hot Spot. In Petrology (pp. 163–187). Springer Berlin Heidelberg. https://doi.org/10.1007/978-3-642-38800-2_8
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