I am a geophysicist, and I study the structure of oceanic tectonic plates. I am currently a Fossett Postdoctoral Fellow in the Department of Earth and Planetary Sciences at Washington University in St. Louis. Previously, I got my PhD in marine geophysics from the MIT-WHOI Joint Program in Oceanography.
I am interested in seismology, fault mechanics, plate boundary processes, and the structure and evolution of oceanic lithosphere. Below are a few current and past projects:
The oceanic LAB in the central Pacific
The mechanical contrast between the rigid lithosphere and ductile asthenosphere is a key feature of plate tectonics, but the nature of the lithosphere-asthenosphere boundary (LAB) remains poorly understood. Receiver function techniques can be used to image upper mantle seismic discontinuities such as the Gutenberg or G discontinuity, which is potentially associated with the oceanic LAB. Applying receiver function techniques to marine seismic data presents particular challenges: data is sparse, and noise in the marine environment severely limits the usable frequencies. We are using S-to-P receiver functions and extended-time multitaper methods to study the oceanic upper mantle beneath the NoMelt array.
Pacific upper-mantle anisotropy from NoMelt
Mantle corner flow beneath mid-ocean ridges is expected to align olivine crystals in the upper mantle into a coherent fabric, thereby making the oceanic upper mantle seismically anisotropic. Seismic refraction data from the NoMelt OBS array in the central Pacific provide constraints on azimuthal anisotropy in 70 Ma, relatively undisturbed oceanic lithosphere. Further, the data indicate that there are anisotropic vertical velocity gradients in the shallow mantle, suggesting that extrinsic sources of anisotropy (such as aligned cracks or other structures) are present. You can read more about this work here (in science language) or here (with a little less jargon).
Controls on mid-ocean ridge normal fault seismicity
Mid-ocean ridge normal faults slip both seismically and aseismically, and the ratio of seismic to aseismic slip has been observed to vary across plate spreading rates. We use rate-and-state friction models to simulate seismic cycles on normal faults and investigate controls on fault behavior that might produce these variations in fault behavior. Our models suggest that the partitioning of seismic and aseismic fault slip is controlled by fault geometry and thermal structure. More about this work can be found here.
Modeling seismic reflection imaging for steeply-dipping faults
Lineations on the ocean floor are the surface expression of bending-related faults near subduction zones. Such faults, as permeable pathways for fluid flow, have implications for the fluid budgets of arc volcanoes. However, high angle faults are difficult to image using seismic reflection. Synthetic seismograms allow us to test whether we should be able to see such faults at depth in seismic images.
Wavelength-dependence of emissivity for shock-compressed iron
Temperatures of shock-compressed materials have been measured using spectral radiance. The wavelength dependence of emissivitiy must be taken into account for calculations of temperature from optical measurements. Reanalyzing the data of Bass et al.  with wavelength-dependent emissivity gives a high-pressure melting temperature for iron that agrees with other experimental and theoretical results. This work was done with Dion Heinz at the University of Chicago.
A general-audience view of a chunk of my thesis research can be found in the 2018 student issue of Oceanus: How is the seafloor made?
I wrote a blog post for AGU's science policy blog, The Bridge, as a student volunteer at the 2018 Fall Meeting, which you can read here: What does it mean for Science to "stand for" something?
If you're more into audio than written text, I told a science-y tale at the Story Collider show at AGU in 2017 which you can listen to over here.
I also wrote a few short pieces for my graduate program's student blog:
- The erstwhile king of Siluria
- A brief history of the Wide Receiver Functions
- Harry Potter and the 12-minute conference talk
- SCARF 2017 cruise recap
You can occasionally find me writing even shorter science-related things on twitter @tellurianite.
Research occupies the vast majority of my time, but even postdocs occasionally do things other than read papers and debug code. I imagine that it would be difficult to stay sane without some hobbies. Mine have, at various times, included running, quilting, playing carillon, librarian-ing, and choral singing. I'm always happy to talk about patchwork, bells, Renaissance choral music, or the merits of the Dewey Decimal system.
hmark (at) wustl.edu
Washington University in St. Louis
Dept. of Earth and Planetary Sciences
Campus Box 1169
1 Brookings Drive
St. Louis, MO 63130
MIT EAPS profile