Abstract:
This thesis presents three studies which apply geophysical tools to the task of better understanding
mantle melting phenomena at the upper and lower boundaries of the mantle. The
first study uses seafloor bathymetry and small variations in the gravitational acceleration
over the Hawaii-Emperor seamount chain to constrain the changes in the igneous production
of the hot spot melting in the mantle which has created these structures over the past 80 My.
The second study uses multichannel seismic reflection data to constrain the location and
depth of axial magma chambers at the Endeavour Segment of the Juan de Fuca spreading
ridge, and then correlates these magma chamber locations with features of the hydrothermal
heat extraction system in the upper crust such as microseismicity caused by thermal
cracking and high temperature hydrothermal vent systems observed on the seafloor. The
third study uses two-dimensional global pseudospectral seismic wave propagation modeling
to characterize the sensitivity of the SPdKS seismic phase to two-dimensional, finite-width
ultra-low velocity zones (ULVZs) at the core-mantle boundary. Together these three studies
highlight the dynamic complexities of melting in the mantle while offering new tools to
understand that complexity.
