Rocks and Water


My research mostly pertains to faulting and lithospheric deformation. I have worked on this on a variety of spatial and temporal scales, from seconds (looking at earthquake deformation) to millions of years (rift evolution). I am also involved in the maintanence of a couple databases of active faults in Himalaya and Tibet and in South America.

Right now, my work is mostly focused on the relationship between stresses from topography and faulting. It's an understudied topic, and one that has a lot of potential, because topographic stresses are both large and relatively easy to estimate (compared to tectonic stress, or earthquake stress drop, or what have you).

I have a pretty multifaceted background, especially with regards to techniques, but strongly favor field and computer work. Currently, the questions I am investigating are best answered through computation, so I don't get out much (sigh). But at least I'm not doing lab work!


(chronological-ish order)

currently (perpetually?) unfinished list

Topographic stresses and their effects on earthquakes and faulting

This is really cool and I'll write about it more in the future. Basically, we are developing methods to calculate the stresses in the upper crust induced by topography, and then using those stresses to get other constraints on tectonic stresses, fault friction, etc., in the crust. We are also looking into how those stresses interact with tectonic stresses during earthquakes. Preliminary results from the 2008 Wenchuan and 2005 Pakistan earthquakes suggest that topographic stresses can significantly affect the coseismic slip distribution during the earthquakes, and in non-inuitive ways (if your intuition is like mine). This is cool in and of itself, but also may give us more insight into the processes and dynamics of earthquake ruptures. I presented this work at AGU Fall 2013. The slideshow is here.

Furthermmore, the stresses on the fault from topography can be used to help estimate the tectonic stresses, especially when the topographic stresses are substantial. We (Eric Hetland and myself) developed the methods to do this while working on the 2008 Wenchuan earthquake. We have a paper accepted in Journal of Geophysical Research about this (pdf here; links to the JGR page and formatted article will be provided as they're available).

I have written a lot of code to do these sorts of calculations, and am open-sourcing things once they aren't embarrassingly messy. For example, the code to perform the topographic stress calculations and to resolve stresses on fault planes is on github.

Extensional history of the South Snake Range Detachment

I am working with Sarah Evans at UNLV doing thermochronological modeling with Pecube of the South Snake Range Detachment in eastern Nevada. She has collected a lot of (U-Th)/He data, which we are combining with published fission track data.

Low-angle normal fault earthquake likelihood

This was a fun little project that was published in Geophysical Research Letters. In it, we (myself and Eric Hetland) mapped all of the known subareal low-angle normal faults and then calculated the maximum likelihood of catching one in the act of rupturing in some short time period (which we haven't really done in the modern earthquake focal mechanism catalogs). Then, we used Bayesian methods to show how to quantitatively adjust our beliefs about low-angle normal fault seismicity in light of both observations of no significant low-angle normal fault seismicity in the catalogs, and the likelihood of actually observing this phenomenon, should it be real.

North Andean tectonics

Rifting and basin inversion in the Eastern Cordillera, Colombia

I did a short project with The Instituto Colombiano del Petroleo (the research wing of Ecopetrol) doing thermochronologic modeling of a very extensive thermochronology database in the eastern Cordillera. We were modeling mostly Mesozoic basin development followed by Cenozoic contraction, including changes in contraction rate through time. Cool project, but I think we pushed Pecube (the modeling software) to much more complicated fault geometries than it is meant for, so we didn't push to publish the results (which are already pretty well constrained by balanced cross sections). The results are going to be used to compare against a forthcoming modeling program by that uses 2D-Move sections to do thermochron modeling.

Active faults in the northern Andes and oblique convergence

This was a project headed by Gabriel Veloza. We (mostly Gabriel) made a big database of active faults in the northern Andes, and then he and I compiled all of the GPS data for the region and showed how the regional fault kinematics (shortening/thrusting to the trench, strike-slip faulting parallel to the trench, extension where there are changes in the convergence obliquity direction) that are seen in faults, earthquakes and GPS data are all quite well explained by oblique convergence between the subducting Nazca plate and the overriding South American plate. Mike Taylor and Andreas Mora contributed a lot to the interpretation and provided guidance.

Himalayan-Tibetan Rifting

A lot of work (most of my dissertation, plus a couple of MS theses by my colleagues, and a bit of help from our friends) went into this. We worked on this from a variety of perspectives.

Oblique convergence

The first was focused on Himalayan rifting. When we started the project, there were several models seeking to explain how and why the Himalaya exhibited arc-parallel extension. We took the four most prominent ones, developed tests for each based on geodetic and geologic predictions made by each model, and then tested them all by analyzing all the available published GPS data, and geologic data where applicable (such as location and total offset of key faults). We concluded that a model of variably-oblique convergence between India and the Himalayan arc best described the 'modern' (late Miocene-present?) deformation. The study was published in Geosphere in 2011 (pdf).

Recently (1 December 2013), a new paper by Mike Murphy, Mike Taylor (my Ph.D. advisor) and collaborators came out in Nature Geoscience, in which they find more field evidence for the influence of oblique convergence in faults in central- western Nepal. This work was bolstered by numerical modeling results by Dave Whipp and Chris Beaumont showing how increasing along-strike convergence obliquity can explain the arc-parallel extension and translation seen in the central-western Himalaya.

I also have a project working on the late Quaternary slip rate history of the Karakoram fault at Menci (near the southeastern end of the KF), but haven't published anything on it yet (still waiting on the data). It was super fun digging the cosmo pits, though. The site has multiple offset features of different ages for some of the fault strands, and I wrote a Monte Carlo-based Python program that takes sets of arbitrary PDFs of ages and offsets (these don't have to be Gaussian or whatever; they can come straight from the map and dating results), and calculates slip and slip rate histories through time, with confidence intervals.

South Tibetan and Himalayan long-term rift histories

South Tibet and the Himalayan hinterland is known for actively extending, and because the area is in an active contractional orogen, is an archetype of synconvergent extension. There are a handful of very well-developed rifts, many of which contain metamorphic core complexes. Because the rifts are active, and the area is pretty cold and dry and mostly unvegetated, the fault scarps at the rangefronts are well-preserved. This makes it an ideal location to study rifting and orogenic processes.

My colleagues and I have worked on this, mostly with the lens/tools of bedrock mapping and thermochronology, and neotectonic mapping and cosmogenic nuclide dating. The former gives insight into million-year timescales of deformation, and the latter into thousands to hundreds of thousands of year timescales. The neotectonics is still a work in progress, and it's not mostly my work.

South Lunggar Rift

The big half of my dissertation involved bedrock and Quaternary mapping of the South Lunggar rift in southwestern Tibet. This was a great project; my advisor and his buddies had done a little work in the North Lunggar rift to the north, but the rift to the south (on the other side of some passes) was completely unstudied, except for some InSAR and teleseismic work done on the 2008 M6.8 Zhongba earthquake, which occurred on the Palung Co fault in the rift.

So I got to take a basically unknown area and bring it into the 21st century, knowledge-wise. It was a lot of work, but it was a wonderful experience. We showed that the rift was a horst with two rift basins on either side, and the north(west)ern part of the horst is an active metamorphic core complex, with a well-developed mylonitic shear zone, fault scarps in moraine at the base with over a hundred meters of cumulative offset, etc. We did zircon (U-Th)/He dating and thermal modeling that showed that rifting initiated in the mid- Miocene at slow rates (< 1 mm/a) and then sped up dramatically at ~8 Ma to about 2.5-3 mm/a, when the South Lunggar detachment and core complex switched on. We published a paper in Tectonics in Oct. 2013 about it (pdf). Good stuff!

North Lunggar Rift

My good friend and colleague Kurt Sundell headed up a similar project to my South Lunggar Rift in the North Lunggar Rift, to the north. There was a little more mapping done previously in the range, so Kurt really focused on thermochronology. We published the work in Tectonics in 2013 (pdf).

Lunggar Rifting and Indian underthrusting

One of the cooler things to come out of the Lunggar Rift work was that extension in the rifts clearly accelerated well after rifting initiated (by millions of years). This was evident in both my modeling with Pecube and with Kurt's 1.5-ish-dimensional modeling. But because we used different techniques, we weren't able to directly compare our results. Therefore, I went through and re-modeled all of the North Lunggar thermochronological data with Pecube. When combined with results from the south, it became evident that the timing of acceleration propagates north; so basically, there is a wave of rapid extension that is moving northward. This wave tracks in front of the northern tip of India, and our interpretation is that crustal thickening at depth is causing crustal extension near the surface as the orogen maintains an equilibrium between horizontal, tectonic forces and vertical, gravitational ones. We published this work in Nature Geoscience in February 2015 (pdf).

2010 Sierra El Mayor - Cucapah earthquake fault scarp LiDAR measurement

This was a fairly short project for me. I helped do LiDAR scans of a segment of the Cucapah rupture, and some data management. Colleagues at UC Davis (mostly Austin Elliott and Peter Gold) have done most of the analysis, which is differencing the yearly scans of the fault to quantify fault scarp degradation patterns and rates.

Nicaraguan Geodesy and Tectonics

My MS thesis at University of Arkansas, with Glen Mattioli. We knew that the Nicaraguan forearc was translating quite rapidly (>10 mm/yr) relative to the rest of the country, but it wasn't clear where the faults that accommodated this motion were. I set up several transects of arc-perpendicular GPS sites over several tens of km to demarcate the shear zone (one or several faults) and get a better estimate of the slip rates. Turns out that the fault is right under the volcanic arc, which is why even though it's mega fast (14-17 mm /yr) it's not visible.

Montserrat syn-eruptive ground deformation

Spent about a year attempting to model huge and rapid surface deformations on Montserrat during the 2003 eruption and dome collapse. Did a lot of work with vertically stacked Mogi sources, but nothing really fit quite right. Turns out that the deformation wasn't real but was caused by the volcanic plume disturbing the atmosphere enough to really screw up the GPS signals. Learned a lot about modeling, though.

last updated 2 March 2015