Primary Research Interests: My research focuses on using high-resolution 2D/3D seismic techniques in conjunction with other geophysical indicators to image, model, and ultimately link shallow geological structure with sediment stress-states and fluid flow. This research is broadly applicable to an array of current geophysical and cross-disciplinary scientific problems including understanding (1) fluid-pressures, slope-failure, and the structure and evolution of continental margins, (2) methane mobilization and its potential impact on climate, (3) the role of seeps and vents in heat/fluid transport and in sustaining diverse chemosynthetic biological seafloor communities and (4) geohazards, with particular emphasis on tsunami generation/propagation. Currently Funded Projects: “Ultra high resolution 3D seismic surveying of active Hydrate Ridge vents to compliment proposed CORKing,” $420,000 granted by NSF-OCE Ocean Drilling Program for a two-year study, starting summer 2008 “Assessing Slope Stability and Tsunami Generation in Students & Postdocs I've Supported as Research Assistants (past/present) DATA EXAMPLES: 3D Seismic Imaging and Fluid Flow Analysis of the (Below:
a movie showing in 3D the seafloor (blue), the base of the hydrate stability
zone signified by a bottom-simulating reflector, or BSR (yellow), and areas
thought to consist of concentrated hydrate (red). The green surfaces mark the
location of eroded buried sediment waves—these features appear to
control the gas distribution on the ridge. The colored surfaces in the image
were created from the migrated 3D volume by using Paradigm Geophysical
Software; the movie file was developed with Matlab. For more information on
these data, see Hornbach et al., GEOPHYSICS,2003; Hornbach et al., JGR, 2008)
Geophysical Analysis of Fluid Flow and Gas Migration at the
(Coming Soon) Submarine Slide and Tsunami Modeling More recently, my research has focused on using seismic
data to constrain the volume and dynamics of submarine landslides, and from
this, back-calculate the possible tsunami generated by these events. Below
show a simplified mudflow (3D Gaussian beam) moving down an idealized
continental slope, and the resulting tsunami this slide generates (program
and images were created in my lab at |
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