Hadean zircon formed due to hydrated ultramafic protocrust melting

Contamination of the Bushveld Complex (South Africa) magmas by basinal brines: Stable isotopes in phlogopite from the UG2 chromitite

Triple Oxygen Isotopes in Evolving Continental Crust, Granites, and Clastic Sediments

Zircon survival in shallow asthenosphere and deep lithosphere

Triple Oxygen ( δ 18 O, Δ 17 O), Hydrogen ( δ 2 H), and Iron ( δ 56 Fe) Stable Isotope Signatures Indicate a Silicate Magma Source and Magmatic-Hydrothermal Genesis for Magnetite Orebodies at El Laco, Chile

Oxygen isotopic investigation of silicic magmatism in the Stillwater caldera complex, Nevada: Generation of large-volume, low-δ 18 O rhyolitic tuffs and assessment of their regional context in the Great Basin of the western United States

Modeling of trace elemental zoning patterns in accessory minerals with emphasis on the origin of micrometer-scale oscillatory zoning in zircon

Iron and Oxygen Isotope Signatures of the Pea Ridge and Pilot Knob Magnetite-Apatite Deposits, Southeast Missouri, USA

Oxygen isotope thermometry reveals high magmatic temperatures and short residence times in Yellowstone and other hot-dry rhyolites compared to cold-wet systems

Linking rapid magma reservoir assembly and eruption trigger mechanisms at evolved Yellowstone-type supervolcanoes

Revised Wonoka isotopic anomaly in South Australia and Late Ediacaran mass extinction

The Fine Gold Intrusive Suite: The roles of basement terranes and magma source development in the Early Cretaceous Sierra Nevada batholith

Supereruptions of the Snake River Plain: Two-stage derivation of low-δ 18 O rhyolites from normal-δ 18 O crust as constrained by Archean xenoliths

Voluminous low δ 18 O magmas in the late Miocene Heise volcanic field, Idaho: Implications for the fate of Yellowstone hotspot calderas

Fragmentation phenomena in populations of magmatic crystals

Rapid generation of both high- and low-δ 18 O, large-volume silicic magmas at the Timber Mountain/Oasis Valley caldera complex, Nevada

Crystal sizes in evolving silicic magma chambers

Formation of low-δ 18 O rhyolites after caldera collapse at Yellowstone, Wyoming, USA