Broadly speaking, my research is focused on how deformation is accommodated across major strike-slip or transpressional boundaries at a variety of lithospheric levels. I also have a scholarship of teaching project examining students' spatial visualization skills.
San Andreas fault
I have been working in central California since 2003 to better understand the distribution of plate boundary deformation along the creeping segment of the San Andreas fault. I have worked with several Carleton undergraduate students on characterizing off-fault deformation adjacent to the Rinconada fault (Zack McGuire '07 and Sarah Crump '10), who worked with Bernie Housen
on their paleomagnetic datasets. More recently, we have been examining deformation at Kettleman Hills (Alice Newman '11 and Amanda Yourd '11, both pictured at right in snake gaitors) and other areas NE of the fault (Peter Lindquist, x'18; Grace Pipes, x'18, and Erin Young-Dahl, x'17).
I collected a suite of structural field data across a mantle shear zone in New Caledonia in 2004. Vasileios Chatzaras
, a post-doc at University of Utrecht, has been adding to this dataset with some lovely microstructural analysis. We are both working with Joshua Davis
to develop models for strain development in the shear zone.
The Troodos ophiolite in Cyprus includes a paleotransform fault exposed at mid-crustal levels, making the region a nice link between upper-crustal deformation in the San Andreas fault and mantle deformation recorded in New Caledonia. I've worked with Chelsea Scott '11, Chelsea Wagner '14, and Sarah Alexander '14 on various projects in the ophiolite.
I have had two field seasons in Iceland collecting paleomagnetic data near the Husavik-Flatey fault, a transform that offsets segments of the Mid-Atlantic ridge that happens to be exposed on land in northern Iceland. I've worked with Andrew Horst, at my alma mater Oberlin College, and Maxwell Brown
from the University of Iceland, along with Will Chapman '16 and Ella Fadely x'18.
Lie groups and statistics
I have also been working with Joshua Davis on applying mathematical methods to geologic problems. Specifically, we have been using Lie theory to model rock deformation. We have been applying our tools to a variety of real geologic datasets. Josh's code for this work can be found here
Geologic structures are inherently three-dimensional. Thus it is important for geologists (both professional and students alike) to be able to picture structures both in 3D space as well as how they might appear on a 2D map, and easily toggle between these two different representations. I developed a series of instructional materials with Eric Horsman
that try to give students frequent practice with different component skills within a geologic context.