Next, Agee and his colleagues used a laser to extract water molecules
trapped within minerals in the meteorite and fed them into a mass spectrometer to calculate the ratio of deuterium, a heavy
isotope of
hydrogen, to ordinary
hydrogen.
To understand how water affects subduction of the oceanic plate, in which layers of different rock types sink into the mantle, the UO team studied
hydrogen isotopes in water contained in tiny blobs of glass
trapped in olivine crystals in basalt.