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Glassy inclusions in magmatic minerals are small amounts of magma trapped in crystallographic defects of the host mineral during crystallization. Their study provides information about the minimum temperature of the liquid at the moment of entrapment, about water pressure, and about the chemical composition of the liquid. The evolution of these inclusions (by exchange between the host mineral and the enclosed liquid) is controlled by the cooling rate of the lava during its movement upward and during its emplacement. This paper presents the basalts of a study of such inclusions in a sample (417D-28-5, 15-19 cm) of Cretaceous basalt recovered from the oceanic basement during DSDP Leg 51.

Glassy Inclusions in Plagioclase and Pyroxene Phenocrysts in the Chilled Margin of a Pillow Lava from Hole 417D, Deep Sea Drilling Project