G.O. Fridleifsson R.A. Zierenberg E.C. Pope A.K. Mortensen A. Gudmundsson Jacob B. Lowenstern N.E. Marks L. Owens D.K. Bird M. Reed N.J. Olsen Peter Schiffmant W.A. Elders 2011 <p><span>Magma flowed into an exploratory geothermal well at 2.1 km depth being drilled in the Krafla central volcano in Iceland, creating a unique opportunity to study rhyolite magma in situ in a basaltic environment. The quenched magma is a partly vesicular, sparsely phyric, glass containing ∼1.8% of dissolved volatiles. Based on calculated H</span>₂<span>O-CO</span>₂<span>&nbsp;saturation pressures, it degassed at a pressure intermediate between hydrostatic and lithostatic, and geothermometry indicates that the crystals in the melt formed at ∼900 °C. The glass shows no signs of hydrothermal alteration, but its hydrogen and oxygen isotopic ratios are much lower than those of typical mantle-derived magmas, indicating that this rhyolite originated by anhydrous mantle-derived magma assimilating partially melted hydrothermally altered basalts.</span></p> application/pdf 10.1130/G31393.1 en Geological Society of America Origin of a rhyolite that intruded a geothermal well while drilling at the Krafla volcano, Iceland article