title: Seismic detection of the summit magma complex of kilauea volcano, hawaii.
abstract: Application of simultaneous inversion of seismic P-wave arrival time data to the investigation of the crust beneath Kilauea Volcano yields a detailed picture of the volcano's heterogeneous structure. Zones of anomalously high seismic velocity are found associated with the volcano's rift zones. A low-velocity zone at shallow depth directly beneath the caldera coincides with an aseismic region interpreted as being the locus of Kilauea's summit magma complex.
authors.forename: C H
authors.initials: CH
authors.lastname: Thurber